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Every parcel of goods shipped across the Atlantic, from the early modern era through the nineteenth century (and beyond), was accompanied by a unique bill of lading. The bill of lading, an essential piece of commercial paperwork, attested that a certain set of goods had been “shipped in good order” and reminded the shipmaster that it was his job to keep them that way. Legally speaking, the bill of lading was a con- tract, a receipt, and a document of title, all in one. Though the legal power of bills of lading depended entirely on their text, American bills nevertheless began in the early eighteenth century to feature decorations, embellishments, and illustrations. The most popular was a ship sailing inside the embellished letter S of the word Shipped. This image, and others like it, helped the bills’ bearers visualize how material objects were caught up in conceptual frameworks of ownership and nationality. Such images thereby strengthened connections among objects, owners, laws, and nations. During the eighteenth and nineteenth centuries, new visual elements, such as flags, human figures, and seascapes, began to appear on American bills of lading, revealing evolving visions of the relationships among commercial goods, vessels, people, nations, and institutions. [ABSTRACT FROM AUTHOR]

From ten years of observations of the Atlantic meridional overturning circulation at 26° N (MOC, 2004-2014), we revisit the question of flow compensation between components of the circulation. Contrasting with early results from the observations, transport variations of the Florida Current (FC) and upper mid-ocean transports (UMO, top 1000 m east of the Bahamas) are now found to compensate on sub-annual timescales. A deep baroclinic response to wind-forcing (Ekman transport) is also found in the lower North Atlantic Deep Water (LNADW, 3000-5000 m) transport. The observed compensation between the FC and UMO transports is associated with horizontal circulation and means that their individual variability does not project onto the MOC. In contrast, covariability between Ekman and the LNADW transports does contribute to overturning. On longer timescales, the southward UMO transport has continued to strengthen, resulting in a continued decline of the MOC. Most of this interannual variability of the MOC can be traced to changes in isopycnal displacements on the western boundary, within the top 1000 m and below 2000 m. Substantial trends are observed in isopycnal displacements in the deep ocean, underscoring the importance of deep boundary measurements to capture the variability of the Atlantic MOC. [ABSTRACT FROM AUTHOR]

We use an eddy-resolving, regional ocean biogeochemical model to investigate the main variables and processes responsible for the climatological spatio-temporal variability of pCO2 and the air--sea CO2 fluxes in the southwestern Atlantic Ocean. Overall, the region acts as sink of atmospheric CO2 south of 30° S, and is close to equilibrium with the atmospheric CO2 to the north. On the shelves, the ocean acts as a weak source of CO2, except for the mid/outer shelves of Patagonia, which act as sinks. In contrast, the inner shelves and the low latitude open ocean of the southwestern Atlantic represent source regions. Observed nearshore-to-offshore and meridional pCO2 gradients are well represented by our simulation. A sensitivity analysis shows the importance of the counteracting effects of temperature and dissolved inorganic carbon (DIC) in controlling the seasonal variability of pCO2. Biological production and solubility are the main processes regulating pCO2, with biological production being particularly important on the shelf regions. The role of mixing/stratification in modulating DIC, and therefore surface pCO2 is shown in a vertical profile at the location of the Ocean Observatories Initiative (OOI) site in the Argentine Basin (42° S, 42° W). [ABSTRACT FROM AUTHOR]

Oscillations of ocean pH are largely unknown in coastal environments and ocean acidification studies often do not account for natural variability yet most of what is known about marine species and populations is found out via studies conducted in near shore environments. Most experiments designed to make predictions about future climate change scenarios are carried out in coastal environments with no research that takes into account the natural pH variability. In order to fill this knowledge gap and to provide reliable measures of pH oscillation, seawater pH was measured over time using moored pH sensors in four contrasting phytocenoses typical of the north Atlantic subtropical region. Each phytocenosis was characterized by its predominant engineer species: (1) Cystoseira abies-marina, (2) a mix of gelidiales and geniculate corallines, (3) Lobophora variegata, and (4) encrusting corallines. The autonomous pH measuring systems consisted of a pH sensor; a data logger and a battery encased in a waterproof container and allowed the acquisition of high-resolution continuous pH data at each of the study sites. The pH variation observed ranged by between 0.09 and 0.24 pHNBS units. A clear daily variation in seawater pH was detected at all the studied sites (0.04-0.12 pHNBS units). Significant differences in daily pH oscillations were also observed between phytocenoses, which shows that macroalgal communities influence the seawater pH in benthic habitats. Natural oscillations in pH must be taken into account in future ocean acidification studies to put findings in perspective and for any ecological recommendations to be realistic. [ABSTRACT FROM AUTHOR]

Trace element incorporation into foraminiferal shells (tests) is governed by physical and chemical conditions of the surrounding marine environment and therefore foraminiferal geochemistry provides a means of palaeoceanographic reconstructions. With the availability of high spatial resolution instrumentation with high precision, foraminiferal geochemistry has become a major research topic over recent years. However, reconstructions of past bottom water oxygenation using foraminiferal tests remain in their infancy. In this study we explore the potential of using Mn/Ca determined by Secondary Ion Mass Spectrometry (SIMS) as well as by Flow-Through Inductively Coupled Plasma Optical Emission Spectroscopy (FT-ICP-OES) in the benthic foraminiferal species Eu- buliminella exilis as a proxy for recording changes in bottom water oxygen conditions in the low latitude NE Atlantic upwelling system. Furthermore, we compare the SIMS and FT-ICP-OES results with published Mn/Al in the bulk sediment from the same sediment core. This is the first time that benthic foraminiferal Mn/Ca is directly compared with Mn/Al in the bulk sediment, which largely agree on the former oxygen conditions. Samples were selected to include different productivity regimes related to Marine Isotope Stage 3 (35-28 ka), the Last Glacial Maximum (28-19 ka), Heinrich Event 1 (18-15.5 ka), Bølling Allerød (15.5-13.5 ka) and the Younger Dryas (13.5-11.5 ka). Foraminiferal Mn/Ca determined by SIMS and FT-ICP-OES are comparable. Mn/Ca was higher during periods with high primary productivity, such as during the Younger Dryas which indicates low oxygen conditions. This is further supported by the benthic foraminiferal faunal composition. Our results highlight the proxy potential of Mn/Ca in benthic foraminifera from upwelling systems for reconstructing past variations in oxygen conditions of the sea floor environment as well as the need to use it in combination with other proxy records such as faunal assemblage data. [ABSTRACT FROM AUTHOR]

Cold-water corals are widely considered as important structural components of benthic habitats, potentially enhancing local abundance in a variety of fish and invertebrate species. Yet, current knowledge of the taxonomic diversity and distribution patterns of these vulnerable, slow-growing organisms is scarce and fragmented, limiting the effectiveness of spatial management and conservation measures. We have conducted an exhaustive compilation of records of alcyonaceans, antipatharians, scleractinians and stylasterids available until the present day to assess the diversity, distribution, and spatial structure of coral assemblages in the Azores Exclusive Economic Zone (EEZ). The resulting database comprises 2501 entries concerning historical oceanographic expeditions and other published sources, as well as recent data from longline bycatch. Our taxonomic inventory appears to be fairly complete for the explored habitats, accounting for 164 species (79 alcyonaceans, 58 scleractinians, 18 antipatharians and 9 stylasterids), nine of which were new records. The Azores EEZ harbours a mixed coral fauna with several zoogeographic origins, showing the closest affinity with the Lusitanian--Mediterranean region. Very few apparent endemics were found (14%), and only in part supported by consistent sampling. Coral diversity is particularly high between 300 and 900m depths, in areas recognized as traditional fishing grounds or exploitable fish habitat within the 100-mile limit of the EEZ. The composition of coral assemblages shows significant geographical structure among longitudinal sections of the study area at comparable depths (100-1500m). There is no evidence of a possible role of the Mid-Atlantic Ridge or latitudinal effects underlying this pattern, which suggests that it may instead reflect assemblage variability among features. Stronger changes in species composition were found along the bathymetric gradient. Notwithstanding the mix of partially overlapping steno- and eurybathic species that characterize the vertical distribution of corals, there is a distinct transition from shallow (100-600m) to intermediate (600-1000m) depths. The analysis here presented constitutes a valuable contribution for efficient conservation policies of coral-associated vulnerable marine ecosystems and their sustainable use as fishing areas. [ABSTRACT FROM AUTHOR]

The assessment of emission factors for many peatlands is difficult, and reliable data on the exchange of carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) between soil and atmosphere of these areas is particularly scarce. Reasons for this are the multitude of soil and land use combinations that control greenhouse gas exchange and the high effort associated with data acquisition. We investigated the greenhouse gas exchange of a peat bog restoration sequence over a period of 2 yr (July 2007-June 2009) in an Atlantic raised bog in Northwest Germany. We set up three sites representing different land use intensities: intensive grassland (mineral fertilizer, cattle manure and 4-5 cuts per year); extensive grassland (no fertilizer or manure, maximal 1 cutting per year); near-natural peat bog (almost no anthropogenic influence). We obtained seasonal and annual estimates of greenhouse gas exchange based on closed chamber measurements. CH4 and N2O fluxes were recorded bi-weekly, CO2 NEE determinations were carried out 3-4 weekly. To get annual sums the CH4 and N2O fluxes were interpolated linearly while NEE was modelled. The intensive grassland site emitted 548±169gCO2-Cm-2 in the first and 817±140gCO2-Cm-2 in the second year. The extensive grassland site showed a slight uptake in the first year (-148 ± 143gCO2-Cm-2), and a small emission of 88±146gCO2-Cm-2 in the second year. In contrast to these agriculturally used sites, the near-natural site took up CO2-C in both years(-8±68gCO2-Cm-2 and -127±53gCO2-Cm-2). Under consideration of N2O and CH4 exchange, the total average greenhouse warming potential (GWP) for 2008 amounts to 441 ±157gm-2,14±152gm-2 and 31 ±68gm-2 CO2-C-equivalent for the intensive grassland, the extensive grassland and the near-natural site, respectively. Despite inter-annual variability, rewetting contributes considerably to mitigating GHG emission from formerly drained peatlands. Already extensively used grassland on moderately drained peat approaches the carbon sequestration potential of near-natural sites, albeit it may oscillate between being a small sink and being a small source depending on interannual climatic variability. [ABSTRACT FROM AUTHOR]

The Eastern Tropical North Atlantic (ETNA) is an open ocean region with little input of terrestrial dissolved organic matter (DOM), suggesting that pelagic production has to be the main source of DOM. Inorganic nitrogen (DIN) and phosphorus (DIP) concentrations affect pelagic production, leading to DOM modifications. The quantitative and qualitative changes in DOM are often estimated by its optical properties. Colored DOM (CDOM) is often used to estimate dissolved organic carbon (DOC) concentrations by applied techniques, e.g. through remote sensing, whereas DOM properties, such as molecular weight, can be estimated from the slopes of the CDOM absorption spectra (S). Fluorescence properties of CDOM (FDOM) allow discriminating between different structural CDOM properties. The investigation of distribution and cycling of CDOM and FDOM was recognized to be important for understanding of physical and biogeochemical processes, influencing DOM. However, little information is available about effects of nutrient variability on CDOM and FDOM dynamics. Here we present results from two mesocosm experiments conducted with a natural plankton community of the ETNA, where effects of DIP (''Varied P") and DIN ("Varied N") supply on optical properties of DOM were studied. CDOM accumulated proportionally to phytoplankton biomass during the experiments. S decreased over time indicating accumulation of high molecular weight DOM. In Varied N, an additional CDOM portion, as a result of bacterial DOM reworking, was determined. It increased the CDOM fraction in DOC proportionally to the supplied DIN. The humic-like FDOM component (Comp.1) was derived by bacteria proportionally to DIN supply. The bound-to-protein amino acid-like FDOM component (Comp.2) was released irrespectively to phytoplankton biomass, but depending on DIP and DIN concentrations, as a part of an overflow mechanism. Under high DIN supply, Comp.2 was removed by bacterial reworking processes, leading to an accumulation of humic-like Comp.1. No influence of nutrient availability on amino acid-like FDOM component in peptide form (Comp.3) was observed. Comp.3 potentially acted as an intermediate product during formation or degradation Comp.2. Our findings suggest that changes in nutrient concentrations may lead to substantial responses in the quantity and "quality" of optically active DOM and, therefore, might bias results of the applied techniques for an estimation of DOC concentrations in open ocean regions. [ABSTRACT FROM AUTHOR]

Artificial drainage of peatlands causes dramatic changes in the release of greenhouse gases and in the export of dissolved carbon (C) and nutrients to downstream ecosystems. Rewetting anthropogenically altered peatlands offers a possibility to reduce nitrogen (N) and C losses. In this study, we investigate the impact of drainage and rewetting on the cycling of dissolved C and N as well as on dissolved gases over a period of 1 yr and 4 month, respectively. The peeper technique was used to receive a high vertical sampling resolution. Within one Atlantic bog complex a near natural site, two drained grasslands sites with different mean water table positions, and a former peat cutting area rewetted 10 yr ago were chosen. Our results clearly indicate that drainage increased the concentration of dissolved organic carbon (DOC), ammonia, nitrate and dissolved organic nitrogen (DON) compared to the near natural site. Drainage depth further determined the release and therefore the concentration level of DOC and N species, but the biochemical cycling and therefore dissolved organic matter (DOM) quality and N species composition were unaffected. Thus, especially deep drainage can cause high DOC losses. In general, DOM at drained sites was enriched in aromatic moieties as indicated by SUVA280 and showed a higher degradation status (lower DOC to DON ratio) compared to the near natural site. At the drained sites, equal C to N ratios of uppermost peat layer and DOC to DON ratio of DOM in soil solution suggest that the uppermost degraded peat layer is the main source of DOM. Nearly constant DOC to DON ratios and SUVA280 values with depth furthermore indicated that DOM moving downwards through the drained sites remained largely unchanged. DON and ammonia contributed most to the total dissolved nitrogen (TN). The subsoil concentrations of nitrate were negligible due to strong decline in nitrate around mean water table depth. Methane production during the winter months at the drained sites moved downwards to areas which were mostly water saturated over the whole year (> 40 cm). Above these depths, the recovery of the [ABSTRACT FROM AUTHOR]

This paper contributes to the literature on payments for slave sales in the later phase of the British slave trade. It analyses the procedures used in the ‘guarantee’ system in transatlantic slaving whereby merchants in British ports forged close connections with African factors in British America and with British businessmen who guaranteed to pay the factors’ bills presented as payments for slave sales. This was an important institutional procedure in the history of the transatlantic slave trade. Though the ‘guarantee’ system has been explained in outline in previous studies, the case study presented here offers the most detailed appraisal of this system. Examining the British slave trade to Jamaica in 1790s, then the most significant disembarkation centre for enslaved people taken on British vessels, the paper explains the coordination necessary between groups of British merchants, their African factors in Jamaica and their British guarantee in order to secure payments for slave sales at a time of considerable volatility in the demand for slaves in Jamaica. The paper suggests that cooperation between merchants in different British ports in connection with the slave trade is as worthy of investigation as the rivalry between the British ports involved in the ‘Guinea’ traffic. [ABSTRACT FROM PUBLISHER]

Previous work in the mud volcanoes from the Gulf of Cadiz revealed a high number of chemosymbiotic species, namely bivalves and siboglinid polychaetes. In this study we give an overview of the distribution and life styles of those species in the Gulf of Cadiz, determine the role of autotrophic symbionts in the nutrition of selected species using stable isotope analyses (δ13C, δ15N and δ34S) and investigate the intra-specific variation of isotope signatures within and between study sites. Twenty siboglinid and nine bivalve chemosymbiotic species have been identified and were found living in fifteen mud volcanoes during our studies. Solemyids bivalves and tubeworms of the genus Siboglinum are the most widespread, whereas other species were found in a single mud volcano (e.g. "Bathymodiolus" mauritanicus) or restricted to deeper mud volcanoes (e.g. Polybrachia sp., Lamelisabella denticulata). Species distribution suggests that different species may adjust their position within the sediment according to their particular needs and intensity and variability of the chemical substrata supply. Isotopic values found for selected species are in accordance with values found in other studies, with thiotrophy as the dominant nutritional pathway, and with methanotrophy and mixotrophy emerging as secondary strategies. The heterogeneity in terms of nutrient sources (expressed in the high variance of nitrogen and sulphur values) and the ability to exploit different resources by the different species may explain the high diversity of chemosymbiotic species found in the Gulf of Cadiz. This study increases the knowledge of the chemosymbiotic species in the Gulf of Cadiz, highlight the relevance of seep chemoautolithotrophic production in this area and provide a starting point for future trophic ecology studies. [ABSTRACT FROM AUTHOR]

The Gulf of Cadiz is an extensive seepage area in the South Iberian Margin (NE Atlantic) encompassing over 40 mud volcanoes (MVs) at depths ranging from 200 to 4000m. The area has a long geologic history and a central biogeographic location with a complex circulation assuring oceanographic connectivity with the Mediterranean Sea, Equatorial and Northern Atlantic regions. The geodynamics of the region promotes a notorious diversity in the seep regime despite the relatively low fluxes of hydrocarbon-rich gases. We analyse quantitative samples taken during the cruises TTR14, TTR15 and MSM01-03 in seven mud volcanoes grouped into Shallow MVs (Mercator: 350m, Kidd: 500m, Meknès: 700m) and Deep MVs (Captain Arutyunov: 1300m, Carlos Ribeiro: 2200m, Bonjardim: 3000m, Porto: 3900m) and two additional reference sites (ca. 550m). Macrofauna (retained by a 500 µm sieve) was identified to species level whenever possible. The samples yielded modest abundances (70-1567 ind. per 0.25 m²) but a number of species among the highest ever reported for cold seeps. Among the 366 recorded species, 22 were symbiont-hosting bivalves (Thyasiridae, Vesicomyidae, Solemyidae) and tubeworms (Siboglinidae). The multivariate analyses indicated significant differences between Shallow and Deep MVs: The environmental conditions at the Shallow MVs makes them highly permeable to the penetration of background fauna leading to high diversity of the attendant assemblages (H': 2.92-3.94; ES(100): 28.3-45.0; J': 0.685-0.881). The Deep MVs showed, in general, contrasting features but were more heterogeneous (H': 1.41-3.06; ES(100): 10.5-30.5; J': 0.340-0.852) and often dominated by one or more siboglinid species. The rarefaction curves confirmed the differences in biodiversity of Deep and Shallow MVs as well as the approximation of the latter to the reference sites. The Bray--Curtis dissimilarity demonstrated the high β-diversity of the assemblages, especially in pairwise comparisons involving samples from the deeper MVs. Diversity partitioning assessed for species richness, Hurlbert's expected number of species and Shannon--Wiener index confirmed the high β-diversity across different spatial scales (within MVs, between MVs, between Deep and Shallow MVs). We suggest that historical and contemporary factors with differential synergies at different depths contribute to the high α-, β- and γ-diversity of the mud volcano faunal assemblages in the Gulf of Cadiz. [ABSTRACT FROM AUTHOR]

information is provided on the conference titled "Community Libraries: Connecting Readers in the Atlantic World, 1650-1850" sponsored by the British Arts and Humanities Research Council held at the University of Liverpool and the Liverpool Athenaeum in Liverpool, England January 24-25, 2014. Topics, including libraries in the 18th century in the Atlantic Ocean region, the relationship between reading and revolution in the Americas and the reading of travel literature, are discussed.

A bibliography related to history is presented, including the books "Confessing History: Explorations in Christian Faith and the Historian's Vocation," edited by John Fea, John Green and Eric Miller, "Teaching the Transatlantic Eighteenth Century," edited by Jennifer Frangos and Cristobal Silva and "How Well Do Facts Travel? The Dissemination of Reliable Knowledge," edited by Peter Howlett and Mary S. Morgan.

This essay presents the previously unpublished ‘Memoirs’ of Florence Hall, an African-born woman enslaved in early nineteenth-century Jamaica. The brief text describes Hall's childhood in Igboland (now southeastern Nigeria), her enslavement and journey to the Atlantic coast, her experience of the Middle Passage, and her arrival in Jamaica. There, the narrative abruptly cuts off. Evidently, the pages containing the rest of her story were lost. The text was likely written in the early nineteenth century, mediated by planter Robert Johnston, in whose papers the surviving text was found. As one of the only slave trade narratives from an African woman anywhere in the Americas, Hall's ‘Memoirs’ offer a rare opportunity to consider the transatlantic slave trade at its peak from the viewpoint of a female captive. [ABSTRACT FROM PUBLISHER]

The British interest and presence in the South Atlantic Ocean and in South America represent, in the words of Eliga Gould, the kind of “entangled histories” increasingly recognised and studied by scholars of imperial, colonial and maritime history. From the beginning of the eighteenth century, the region was most frequently seen as the “key” to the Pacific Ocean. This paper, however, focuses on the place of this oceanic area, its islands and its coastal littorals in another “gateway zone”: the entrance to, and exit from, Britain's Indian Ocean world and the riches of Asia. The strategic location of various South Atlantic islands and South American colonial entrepôts played on the minds of politicians, policy-makers, publicists and merchants in London, as well as colonial governors and military commanders on station. Drawing on the archival riches of the East India Company, as well as primary published material such as pamphlets and prospectuses, this paper will explore the interaction of the Atlantic and Indian oceans at this maritime fault-line. The discussion will demonstrate, for example, how the “barren and rocky isle” of St Helena, “abandoned to a state of hopeless destitution in the solitude of the ocean,” could be regarded as an “essential part of the British Empire.” And similarly, it will demonstrate how places such as Montevideo, Rio de Janeiro and Tristan da Cunha were regarded in relation to the rising British Empire in Asia. More broadly, the region cannot be understood, this paper suggests, without considering the wider context of British imperial and commercial activity in the period and, more specifically, the growing importance of British trading and political interests in the East Indies. [ABSTRACT FROM PUBLISHER]

The article offers information on the July 17, 2014 to July 19, 2014 conference "London and the Americas, 1492-1812" by the Society of Early Americanists (SEA) at Kingston University in London, England. Topics include the interdisciplinary nature of the conference, the role of network theory in scholarship on the Atlantic Ocean region, and papers on the history of London.

Quillérou, E. and Guyader, O. 2012. What is behind fleet evolution: a framework for flow analysis and application to the French Atlantic fleet – ICES Journal of Marine Science, 69: 1069–1077.The study of fishery dynamics considers national-level fleet evolution. It has, however, failed to consider the flows behind fleet evolution as well as the impact of the dynamics of owners of invested capital on fleet evolution. This paper establishes a general conceptual framework which identifies different vessel and owner flows behind fleet evolution and some relationships between these flows. This descriptive conceptual framework aims to change the current focus on drivers of fleet evolution to drivers of the flows behind fleet evolution. We identify a direct impact of vessel flows on the fleet size and nature, and an indirect impact of the movements of capital owners on the fleet evolution (size and nature). This conceptual framework is illustrated using French Atlantic fleet data over a 15-year period (1994–2008). It is shown that the identified flows vary in size and nature and therefore impact differently on the fleet evolution. This description also shows some dependence of vessel flows on owner dynamics. This relationship should be better taken into account for more effective capacity management. [ABSTRACT FROM PUBLISHER]

This article engages theories of mobility to examine the Royal Mail Steam Packet Company's (RMSPC's) 1851 expansion into South America. Through a focus on cooperative strategies and trans-oceanic connections, the article also considers the interplay between Atlantic and wider world shipping networks. The first part of the paper compares the RMSPC's South American branch to the more established West Indies route, and probes the significance of the Company's expansion into the South Atlantic in light of the RMSPC's perceived national and imperial role. The second part of the paper turns to the RMSPC's cooperative strategies and connections between the Atlantic and the Pacific oceans. Considered as a case study, the RMSPC indicates that the boundaries of British imperial influence incorporated a degree of flexibility during this period, pointing to a need to revise rigid conceptualisations of empire. An argument is also made for the continuing relevance of the Atlantic as a spatial unit during this era, despite the increasingly global connections of the nineteenth-century world. [ABSTRACT FROM PUBLISHER]

This paper examines how and why information moved or failed to move within transatlantic botanical networks in the late eighteenth century. It addresses the problem of how practitioners created relationships of trust, and the difficulties they faced in transferring reputations between national contexts. Eighteenth-century botany was characteristically cross-cultural, cosmopolitan and socially diverse, yet in the 1770s and 1780s the American Revolutionary Wars placed these attributes under strain. The paper analyses the British and French networks that surrounded the Philadelphian plant hunter William Young (1742–1785), to show how botanists and plant collectors created and maintained connections with each other, especially when separated by geographical and cultural distance. It highlights in particular the role played by commercial plant traders, and demonstrates how practitioners used objects to transmit social as well as scholarly information. The transnational circulation of information and knowledge in the Enlightenment was determined by culturally specific judgements about trust, confidence, communication and risk. Despite the prominent role played by material culture within these networks, scholars continued to place high value on face-to-face contact as a means of judging the trustworthiness and cooperation of their agents. [ABSTRACT FROM AUTHOR]

TThis technical paper provides an inventory of, and describes trends in, legal, administrative and management frameworks in place for managing marine capture fisheries in the Western Central Atlantic Fishery Commission (WECAFC) area. This review includes 16 countries and overseas territories and is part of an ongoing process initiated by FAO to report on the state of world marine capture fisheries management. The review identifies a number of challenges in fisheries management, including: inadequate legislation; ad hoc management processes and plans; uncoordinated monitoring and enforcement; non-management-driven scientific information; insufficient stakeholder identification and participation, conflict resolution and fishing capacity measurements; limited incorporation of issues pertaining to the operation of multispecies fisheries and use of the ecosystem approach; unequal application of management tools and measures across fisheries subsectors; and rising fisheries management costs coupled with stagnant budgets for governments. Actions are listed to address the challenges, and specific recommendations are made to address legislative issues, apply participatory approaches and implement a successful fisheries management process. The fifteenth session of WECAFC (March 2014) endorsed the review outcomes and adopted recommendation WECAFC/15/2014/4 "on strengthening fisheries management planning in the WECAFC area". This technical paper aims to inform fishery policy decision-makers, fishery managers and other stakeholders with interest in fisheries in the Wider Caribbean Region. [ABSTRACT FROM AUTHOR]

This paper assesses the merits and drawbacks of several data sets of solar downwelling radiation received at the horizontal surface of the tropical Atlantic Ocean where the magnitude of this radiation and its spatial and temporal variability are not well known. The data sets are compared to quality-controlled measurements of hourly means of irradiance made at five buoys of the PIRATA network for the period 2012-2013. The data sets comprise the re-analyses MERRA-2 and ERA5, and three satellite-derived data sets: HelioClim-3v5, SARAH-2 and CAMS Radiation Service v2. It was found that the re-analyses MERRA-2 and ERA5 often report cloud-free conditions while the actual conditions are cloudy, yielding an overestimation of the irradiance in such cases; and reciprocally, they report actual cloud-free conditions as cloudy, yielding an underestimation. The re-analyses exhibit more bias in irradiance in cases of medium and highlevel clouds than for low-level clouds. They correlate well with the hourly means of irradiance (as a whole, correlation coefficients greater than 0.85 for MERRA-2 and 0.89 for ERA5); they correlate very poorly with daily means of irradiance (coefficients of less than 0.48 and 0.59 for MERRA- 2 and ERA5, respectively) and with the hourly and daily clearness indices (coefficients of less than 0.53 and 0.46 for MERRA-2 and less than 0.63 and 0.59 for ERA5). The irradiance pattern at both hourly and daily timescales is spatially distorted by re-analyses, especially for MERRA-2. The three satellite-derived data sets exhibit similar performances between them. The correlation coefficients are greater than 0.95 and 0.78 for irradiance and clearness index, respectively, in most cases for hourly values and 0.90 and 0.88, respectively, for daily values. The relative standard deviation of errors is of the order of 15% for hourly values and 8% for daily values. It is concluded that these data sets reproduce well the dynamics of the irradiance and clearness index at both hourly and daily timescales. They exhibit overestimation, with the lowest biases reached by the CAMS Radiation Service v2 and ranging between 11 and 37Wm-2 depending on the buoy. It is suggested that HelioClim-3v5 and CAMS Radiation Service v2 are suited for reproducing the spatial gradients of the irradiance and reflecting the spatial variability in the irradiance. [ABSTRACT FROM AUTHOR]

Fragments of continental structures are widespread in the North and South Atlantic and almost absent in the central segment of the ocean. This implies that the fragments are related to the geodynamics of the surrounding continents. The fragments are subdivided into two groups: microcontinents and submarine prominences of marginal continental blocks. Both groups are briefly characterized in this paper, and views on mechanisms of their formation are expressed. In my opinion, there is a good reason to believe that this line of research makes a substantial contribution to mobilistic geotectonics. [ABSTRACT FROM AUTHOR]

Purpose – A reliable forecast of hurricane activity in the Atlantic Basin has the potential to help mitigate the economic losses caused by hurricanes. One of the difficult problems is to make reasonable annual forecast of catastrophe losses based on the short record of historical observations. Atmospheric conditions tend to influence tropical cyclone development. Considering the complex interactions among climatological factors, prediction of future hurricane activity is challenging. In this study, the authors are attempting to predict the number of Atlantic hurricanes for a given year based on two different approaches. Design/methodology/approach – In part I, an autoregressive integrated moving average (ARIMA) is used to model a long-run behavior of Atlantic hurricane frequency. The authors present a comparison of CSU's forecast with ARIMA model. Part II focuses on the relationship between the climate signals and hurricane activity and introduces a new approach in including climate indices into the prediction model. In this part, principal components analysis (PCA) is used to identify possible patterns in historical data based on six climate indices measured prior to hurricane season. The objective is to reduce the data set to a smaller set while most of the variability observed in the real data is captured. The variances observed in an orthogonal system indicate the order of contribution of each mode shape. Findings – Results from part I suggest that CSU's forecast model, in general, is superior to results obtained by ARIMA. In part II, the correlation between mode (shapes) and the number of Atlantic hurricanes per year is examined. The resulting relationships show that, for the time interval of 1990 through 2011, PCA-based approach provides better estimates compared to CSU's forecast. Originality/value – The paper presents a unique prediction approach which is simple, relatively accurate and easy to apply. The results of this study show that complex statistical analyses/models do not necessarily provide better forecasts. [ABSTRACT FROM AUTHOR]

This paper examines Gilded Age affluence by focusing on apparently inconsequential decorative goods and assessing how such goods were part of shared transatlantic patterns that reached beyond the Gilded Age and the confines of urban America. The paper focuses on figurines recovered from nineteenth-century sites in London and underscores how the American Gilded Age amplified many early nineteenth-century material patterns and ideological practices that were well-established in the United Kingdom and continued after the height of Gilded Age affluence. This study examines the symbolism of such aesthetically eclectic goods and focuses on the socially grounded imagination that was invested in them borrowing from dominant ideologies and idiosyncratic personal experiences alike. [ABSTRACT FROM AUTHOR]

This paper presents the reconstruction of a climatological series of winter coastal storms on the northern coasts of the Gulf of Cadiz. This series has been put together using information extracted from regional and local Spanish newspapers. It includes all the storms coming from the Atlantic sector that have been detected during the winter season, from October to March, between 1929 and 2005. In order to validate this historical storm series, it has been compared with storms series identified from quasi-observational data and using different wave heights as thresholds to decide what is to be considered as a coastal storm. Nearly 2.6 reports per year about coastal storms are published in the press which correspond to waves of 3.6 m high or more and to prevailing winds from a direction ranging between SSW and WNW. A long- term positive trend has been detected for the complete storm series. If only the instrumental period is analysed, no significant trend is detected. It is suggested that this difference might be associated with the impact of the North Atlantic Oscillation over the occurrence of storms in this area. [ABSTRACT FROM AUTHOR]

Compared with the attention paid to written texts, geographers and others have neglected the spoken word in its many forms, particularly in investigations of the power relations of colonialism and imperialism. This paper argues that considering orality as a series of embodied, situated enunciations, declarations and conversations can provide a basis for historical geographies of the spoken word that engage with representation as practice. Using evidence from the domain of law within the context of Britain's plantation colonies in the Caribbean - particularly Barbados and Jamaica - this paper argues for the significance of the oral culture of empire. This was evident in the ways in which the power of speech - through the rules on oath-taking and evidence-giving - was part of the making of imperial and colonial identities and relationships dividing white and non-white, free and unfree, both within the spaces of plantation societies and in the broader British Atlantic world. The fragility of the identities and relationships made through the spoken word is also demonstrated through a series of moments when changes in the regulation of speech in courts of law were suggested and contested. [ABSTRACT FROM AUTHOR]

The development of appropriate risk and vulnerability reduction strategies to cope with tsunami risks is a major challenge for countries, regions, and cities exposed to potential tsunamis. European coastal cities such as Cadiz are exposed to tsunami risks. However, most official risk reduction strategies as well as the local population are not aware of the probability of such a phenomenon and the potential threat that tsunami waves could pose to their littoral. This paper outlines how tsunami risks, and particularly tsunami vulnerability, could be assessed and measured. To achieve this, a vulnerability assessment framework was applied focusing on the city of Cadiz as a case study in order to highlight the practical use and the challenges and gaps such an assessment has to deal with. The findings yield important information that could assist with the systematic improvement of societal response capacities of cities and their inhabitants to potential tsunami risks. Hazard and vulnerability maps were developed, and qualitative data was obtained through, for example, focused group discussions. These maps and surveys are essential for the development of a people-centred early warning and response system. Therefore, in this regard, the Tsunami Early Warning and Mitigation System in the North Eastern Atlantic, the Mediterranean, and connected seas promoted by the UNESCO-Intergovernmental Oceanographic Commission (IOC) should encompass these assessments to ensure that action is particularly intensified and fostered by those potentially exposed. That means that besides the necessary technical infrastructure for tsunami detection, additional response and adaptation measures need to be promoted -- particularly those that reduce the vulnerability of people and regions exposed -- in terms of national systems. In addition, it is important to develop emergency preparedness and awareness plans in order to create an integrated regional Tsunami EarlyWarning System (TEWS) by 2011. The findings of the paper are based on research conducted within the framework of the EC funded project TRANSFER: "Tsunami Risk ANd Strategies For the European Region", a project that aims to improve the understanding of tsunami processes in the Euro- Mediterranean region, to develop methods and tools to assess vulnerability and risk, and to identify strategies for the reduction of tsunami risks. [ABSTRACT FROM AUTHOR]

The large-scale equatorial circulation known as the Madden–Julian oscillation (MJO) has been shown to impact tropical cyclone activity in several basins around the globe. In this paper, the author utilizes an MJO index created by Wheeler and Hendon to examine its impacts on tropical genesis and intensification in the Atlantic. Large differences in frequency and intensity of tropical cyclone activity are seen, both in the tropical Atlantic as well as in the northwest Caribbean and Gulf of Mexico depending on the MJO phase. Coherent changes in upper- and lower-level winds and relative humidity are likely responsible for these differences. Since the MJO shows potential predictability out to about two weeks, the relationships discussed in this paper may be useful for short-term predictions of the probability of tropical cyclone activity in the Atlantic as a complement to the already available longer-term seasonal predictions. [ABSTRACT FROM AUTHOR]

Small-scale grazing events where sea urchins have grazed kelp forests to barren grounds have been reported all along the NE Atlantic coast. One large-scale event has been reported where kelp forests along the Norwegian and Russian coast were grazed by sea urchins during the early 1970s. The barren ground area has persisted since. Different theories to explain the grazing event have been presented. This paper seeks to sort and summarize earlier published papers and national reports and to critically examine the most important theories presented to explain the grazing event. The conclusion is that the reason for the event is unknown and it is too late to find causes 40 years after it took place. However, new data and new geographical analysis tools provide insight into the extent and consequences of this dramatic event, and show re-vegetation of kelp forests in the southernmost area. Emphasis in future studies should be given to understand the reasons for shifts between the two ecosystem states and take advantage of the ongoing shift. Such basic ecological knowledge could provide an important basis for better understanding the system and further, to understand the extent to which other observed large-scale changes (e.g. climatic changes, fish stock reductions) affect kelp forest-sea urchin interaction. [ABSTRACT FROM AUTHOR]

This paper investigates convective burst (CB) evolution in Weather Research and Forecasting (WRF) Model simulations of two tropical cyclones (TCs), focusing on the relationship between CBs and TC intensity change. Analysis of intensity change in the simulations shows that there are more CBs inside the radius of maximum winds (RMW) during times when the TCs are about to intensify, while weakening/steady times are associated with more CBs outside the RMW, consistent with past observational and theoretical studies. The vertical mass flux distributions show greater vertical mass flux at upper levels both from weaker updrafts and CBs for intensifying cases. The TC simulations are further dissected by past intensity change, and times of sustained intensification have more CBs than times when the TC has been weakening but then intensifies. This result suggests that CB development may not always be predictive of intensification, but rather may occur as a result of ongoing intensification and contribute to ongoing intensification. Abrupt short-term intensification is found to be associated with an even higher density of CBs inside the RMW than is slower intensification. Lag correlations between CBs and intensity reveal a broad peak, with the CBs leading pressure falls by 0-3 h. These relationships are further confirmed by analysis of individual simulation periods, although the relationship can vary depending on environmental conditions and the previous evolution of the TC. These results show that increased convection due to both weak updrafts and CBs inside the RMW is favorable for sustained TC intensification and show many details of the typical short-term response of the TC core to CBs. [ABSTRACT FROM AUTHOR]

The discourse on reparation for African Americans has gained impulse and will continue to gain significance in the future. The reparation scholarship reached new levels since the 1980s due to the impetus from the legislative precedent set by the US Congress in passing the Civil Liberties Act of 1988 which provided the basis for compensation to Japanese Americans interned during the Second World War. As for reparations for Africa and other nations that suffered under the transatlantic slave trade and the European colonialism, there is an absence of political will to articulate demands for reparations for and present them at international forums. This paper examines the existing scholarship on reparation for African America. To understand the key arguments, the paper identified three main broad academic epistemic communities and other subdivisions on reparations for African Americans and Africa. It is hoped that this paper will provide some insights to policy makers and scholars. [ABSTRACT FROM AUTHOR]

This paper describes a new model (method) called Satellite-derived North Atlantic Profiles (SNAP) that seeks to provide a high-resolution, near-real-time ocean thermal field to aid tropical cyclone (TC) forecasting. Using about 139 000 observed temperature profiles, a spatially dependent regression model is developed for the North Atlantic Ocean during hurricane season. A new step introduced in this work is that the daily mixed layer depth is derived from the output of a one-dimensional Price-Weller-Pinkel ocean mixed layer model with time-dependent surface forcing. The accuracy of SNAP is assessed by comparison to 19 076 independent Argo profiles from the hurricane seasons of 2011 and 2013. The rms differences of the SNAP-estimated isotherm depths are found to be 10-25 m for upper thermocline isotherms (29°-19°C), 35-55 m for middle isotherms (18°-7°C), and 60-100 m for lower isotherms (6°-4°C). The primary error sources include uncertainty of sea surface height anomaly (SSHA), high-frequency fluctuations of isotherm depths, salinity effects, and the barotropic component of SSHA. These account for roughly 29%, 25%, 19%, and 10% of the estimation error, respectively. The rms differences of TC-related ocean parameters, upper-ocean heat content, and averaged temperature of the upper 100 m, are ~10 kJ cm−2 and ~0.8°C, respectively, over the North Atlantic basin. These errors are typical also of the open ocean underlying the majority of TC tracks. Errors are somewhat larger over regions of greatest mesoscale variability (i.e., the Gulf Stream and the Loop Current within the Gulf of Mexico). [ABSTRACT FROM AUTHOR]

Copyright of Journal of King Abdulaziz University: Marine Sciences is the property of King Abdulaziz University, Scientific Publishing Centre and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Credit facilitated the intra-US slave trade's growth between 1815 and the financial crisis of the late 1830s. Movement of money across geographic space was the enslavers’ chief challenge, and this article details the process of slaving firms’ building credit and remitting funds with which they constructed supply chains in bondspersons. Slave market development was dependent on US and North Atlantic financial integration and comprised three stages. These included use of the Second Bank of the USA, supplemented by domestic bills of exchange, and culminating in the use of southern state banks with northern correspondent ties, which the financial crisis severed. [ABSTRACT FROM PUBLISHER]

Halocarbons from oceanic sources contribute to halogens in the troposphere, and can be transported into the stratosphere where they take part in ozone depletion. This paper presents distribution and sources in the equatorial Atlantic from June and July 2011 of the four compounds bromoform (CHBr3), dibromomethane (CH2Br2), methyl iodide (CH3I) and diiodomethane (CH2I2). Enhanced biological production during the Atlantic Cold Tongue (ACT) season, indicated by phytoplankton pigment concentrations, led to elevated concentrations of CHBr3 of up to 44.7 and up to 9.2 pmol L-1 for CH2Br2 in surface water, which is comparable to other tropical upwelling systems. While both compounds correlated very well with each other in the surface water, CH2Br2 was often more elevated in greater depth than CHBr3, which showed maxima in the vicinity of the deep chlorophyll maximum. The deeper maximum of CH2Br2 indicates an additional source in comparison to CHBr3 or a slower degradation of CH2Br2. Concentrations of CH3I of up to 12.8 pmol L-1 in the surface water were measured. In contrary to expectations of a predominantly photochemical source in the tropical ocean, its distribution was mostly in agreement with biological parameters, indicating a biological source. CH2I2 was very low in the near surface water with maximum concentrations of only 3.7 pmol L-1. CH2I2 showed distinct maxima in deeper waters similar to CH2Br2. For the first time, diapycnal fluxes of the four halocarbons from the upper thermocline into and out of the mixed layer were determined. These fluxes were low in comparison to the halocarbon sea-to-air fluxes. This indicates that despite the observed maximum concentrations at depth, production in the surface mixed layer is the main oceanic source for all four compounds and one of the main driving factors of their emissions into the atmosphere in the ACT-region. The calculated production rates of the compounds in the mixed layer are 34±65 pmolm-3 h-1 for CHBr3, 10±12 pmolm-3 h-1 for CH2Br2, 21±24 pmolm-3 h-1 for CH3I and 384±318 pmolm-3 h-1 for CH2I2 determined from 13 depth profiles. [ABSTRACT FROM AUTHOR]

Historians have recently turned their attention to the place of masculinity in the politics of early-modern England. This essay widens that exploration to include the imperial settings of Ireland and North America. Drawing upon a range of English- and Irish-language sources – including political treatises, maps, state papers and court poetry – it contends that manhood, as a relational value between men, helped structure the form and character of politics in the metropole, the kingdom of Ireland and the American colonies. In all of those settings, the definition of acceptable male behaviour was different, the effect being that political action and theory in each place took on unique features. Consequently, the essay cautions against studying England and its colonies as distinct units of historical analysis and calls for further exploration of the particularities of colonial settings and their influence on the imperial centre. Moreover, the essay aims to demonstrate that masculinity, particularly contest over its proper expression, is an agent in historical change, in this case helping to shape political theory and practice as England developed into a multiple monarchy and budding imperial power in the sixteenth and early seventeenth centuries. [ABSTRACT FROM AUTHOR]

• Background and Aims Myrcia section Aulomyrcia includes ~120 species that are endemic to the Neotropics and disjunctly distributed in the moist Amazon and Atlantic coastal forests of Brazil. This paper presents the first comprehensive phylogenetic study of this group and this phylogeny is used as a basis to evaluate recent classification systems and to test alternative hypotheses associated with the history of this clade. • Methods Fifty-three taxa were sampled out of the 120 species currently recognized, plus 40 outgroup taxa, for one nuclear marker (ribosomal internal transcribed spacer) and four plastid markers (psbA-trnH, trnL-trnF, trnQ-rpS16 and ndhF). The relationships were reconstructed based on Bayesian and maximum likelihood analyses. Additionally, a likelihood approach, 'geographic state speciation and extinction', was used to estimate region-dependent rates of speciation, extinction and dispersal, comparing historically climatic stable areas (refugia) and unstable areas. • Key Results Maximum likelihood and Bayesian inferences indicate that Myrcia and Marlierea are polyphyletic, and the internal groupings recovered are characterized by combinations of morphological characters. Phylogenetic relationships support a link between Amazonian and north-eastern species and between north-eastern and south-eastern species. Lower extinction rates within glacial refugia suggest that these areas were important in maintaining diversity in the Atlantic forest biodiversity hotspot. • Conclusions This study provides a robust phylogenetic framework to address important ecological questions for Myrcia s.l. within an evolutionary context, and supports the need to unite taxonomically the two traditional genera Myrcia and Marlierea in an expanded Myrcia s.l. Furthermore, this study offers valuable insights into the diversification of plant species in the highly impacted Atlantic forest of South America; evidence is presented that the lowest extinction rates are found inside refugia and that range expansion from unstable areas contributes to the highest levels of plant diversity in the Bahian refugium. [ABSTRACT FROM AUTHOR]

Many coupled general circulation models (CGCMs) suffer from serious model bias in the zonal gradient of sea surface temperature (SST) in the equatorial Atlantic. The bias of the equatorial Atlantic SST (EASST) may affect the interannual variability of the equatorial Atlantic, which in turn may influence the state of the tropical Pacific. In this paper we investigate the impact of the bias and the interannual variability of the EASST on the tropical Pacific in a CGCM. To determine the impact of the interannual variability of the EASST on the tropical Pacific, we compare a run in a fully coupled mode (CTL run) and a run in which the EASST is nudged toward the climatological monthly mean of the SST in the CTL run, but full air-sea coupling is allowed elsewhere (AT_m run). We find that, when the interannual variability of the EASST is excluded, the thermocline depth in the eastern equatorial Pacific is deepened, and the amplitude of the El Niño/Southern Oscillation is reduced by 30 % compared to the CTL run. The impact of the bias of the EASST on the tropical Pacific is investigated by comparing the AT_m run and a run in which the EASST is nudged toward the observed climatological monthly mean SST (AT_o run). It is found that, when the bias of the EASST is removed (i.e. AT_o run), the Gill-Matsuno type response to the warm SST anomalies in the western equatorial Atlantic induces low-level cyclonic anomalies in the eastern South Pacific, which leads to a deeper thermocline and colder SST in the South Pacific as compared to AT_m. The colder SST in the South Pacific reduces the precipitation along the South Pacific convergence zone. Our results of the model experiments demonstrate the importance of the EASST to the tropical Pacific climate. [ABSTRACT FROM AUTHOR]

Since its publication in 1966, Flora Nwapa's Efuru has largely been read as a narrative of women's solidarity. This paper departs from existing criticism by situating Efuru within a genealogy of West African fiction on the relations between Atlantic and African slaving networks. Efuru's exploration of women's subordinations within slaving systems, family sagas, and commodity histories locates women within an Atlantic world-system overtaken by colonialism. By focusing on narrative form, I read Efuru as a dialogue novel in which the author deploys strategies of indirection in order to narrate the disrupted historical relations of the lost Atlantic sphere in which Atlantic and domestic African slaveries were worlded. Such indirection, in turn, responds to the chagrin of African implication in Atlantic networks. [ABSTRACT FROM AUTHOR]

After going unreported in the northwestern Atlantic Ocean for 18 years (1988 to 2006), the Asian tiger shrimp, Penaeus monodon, has recently reappeared in the South Atlantic Bight and, for the first time ever, in the Gulf of Mexico. Potential vectors and sources of this recent invader include: 1) discharged ballast water from its native range in Asia or other areas where it has become established; 2) transport of larvae from established non-native populations in the Caribbean or South America via ocean currents; or 3) escape and subsequent migration from active aquaculture facilities in the western Atlantic. This paper documents recent collections of P. monodon from the South Atlantic Bight and the Gulf of Mexico, reporting demographic and preliminary phylogenetic information for specimens collected between North Carolina and Texas from 2006 through 2012. The increased number of reports in 2011 and 2012, ranging from 102 mm to 298 mm total length, indicates that an adult population is present in densities sufficient for breeding, which is indicative of incipient establishment. Based on these reports of P. monodon, its successful invasion elsewhere, and its life history, we believe that this species will become common in the South Atlantic Bight and Gulf of Mexico in less than 10 years. Penaeus monodon is an aggressive predator in its native range and, if established, may prey on native shrimps, crabs, and bivalves. The impacts of an established P. monodon population are potentially widespread (e.g., alterations in local commercial fisheries, direct and indirect pressures on native shrimp, crab and bivalve populations, and subsequent impacts on the populations of other predators of those organisms) and should be considered by resource managers. The impacts of P. monodon on native fauna and the source(s) or vector(s) of the invasion, however, remain unknown at this time. [ABSTRACT FROM AUTHOR]

Fisheries statistics are known to be underestimated, since they are mainly based on information about commercial fisheries. However, various types of fishing activities exist and evaluating them is necessary for implementing effective management plans. This paper assesses the characteristics and catches of the French European sea bass recreational fishery along the Atlantic coasts, through the combination of large-scale telephone surveys and fishing diaries study. Our results demonstrated that half of the total catches (mainly small fish) were released at sea and that the mean length of a kept sea bass was 46.6 cm. We highlighted different patterns of fishing methods and type of gear used. Catches from boats were greater than from the shore, both in abundance and biomass, considering mean values per fishing trip as well as CPUE. Spearfishers caught the highest biomass of sea bass per fishing trip, but the fishing rod with lure was the most effective type of gear in terms of CPUE. Longlines had the highest CPUE value in abundance but not in biomass: they caught numerous but small sea bass. Handlines were less effective, catching few sea bass in both abundance and biomass. We estimated that the annual total recreational sea bass catches was 3,173 tonnes of which 2,345 tonnes were kept. Since the annual commercial catches landings were evaluated at 5,160 tonnes, recreational landings represent 30% of the total fishing catches on the Atlantic coasts of France. Using fishers' self-reports was a valuable way to obtain new information on data-poor fisheries. Our results underline the importance of evaluating recreational fishing as a part of the total amount of fisheries catches. More studies are critically needed to assess overall fish resources caught in order to develop effective fishery management tools. [ABSTRACT FROM AUTHOR]

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This paper presents an evaluation of the multi-model simulations for the 4th Assessment Report of the Intergovernmental Panel on Climate Change (IPCC) in terms of their ability to simulate the ERA40 circulation types over the Euro-Atlantic region in winter season. Two classification schemes, k-means and SANDRA, have been considered to test the sensitivity of the evaluation results to the classification procedure. The assessment allows establishing different rankings attending spatial and temporal features of the circulation types. Regarding temporal characteristics, in general, all AR4 models tend to underestimate the frequency of occurrence. The best model simulating spatial characteristics is the UKMO-HadGEM1 whereas CCSM3, UKMO-HadGEM1 and CGCM3.1(T63) are the best simulating the temporal features, for both classification schemes. This result agrees with the AR4 models ranking obtained when having analysed the ability of the same AR4 models to simulate Euro-Atlantic variability modes. This study has proved the utility of applying such a synoptic climatology approach as a diagnostic tool for models' assessment. The ability of the models to properly reproduce the position of ridges and troughs and the frequency of synoptic patterns, will therefore improve our confidence in the response of models to future climate changes. [ABSTRACT FROM AUTHOR]

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This paper focuses on diagnosing biases in the seasonal climate of the tropical Atlantic in the twentieth-century simulation of the Community Climate System Model, version 4 (CCSM4). The biases appear in both atmospheric and oceanic components. Mean sea level pressure is erroneously high by a few millibars in the subtropical highs and erroneously low in the polar lows (similar to CCSM3). As a result, surface winds in the tropics are ~1 m s−1 too strong. Excess winds cause excess cooling and depressed SSTs north of the equator. However, south of the equator SST is erroneously high due to the presence of additional warming effects. The region of highest SST bias is close to southern Africa near the mean latitude of the Angola-Benguela Front (ABF). Comparison of CCSM4 to ocean simulations of various resolutions suggests that insufficient horizontal resolution leads to the insufficient northward transport of cool water along this coast and an erroneous southward stretching of the ABF. A similar problem arises in the coupled model if the atmospheric component produces alongshore winds that are too weak. Erroneously warm coastal SSTs spread westward through a combination of advection and positive air-sea feedback involving marine stratocumulus clouds. This study thus highlights three aspects to improve to reduce bias in coupled simulations of the tropical Atlantic: 1) large-scale atmospheric pressure fields; 2) the parameterization of stratocumulus clouds; and 3) the processes, including winds and ocean model resolution, that lead to errors in seasonal SST along southwestern Africa. Improvements of the latter require horizontal resolution much finer than the 1° currently used in many climate models. [ABSTRACT FROM AUTHOR]