12 results on '"Malsale, P"'
Search Results
2. Severe tropical cyclones over southwest Pacific Islands: economic impacts and implications for disaster risk management
- Author
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Deo, Anil, Chand, Savin S., McIntosh, R. Duncan, Prakash, Bipen, Holbrook, Neil J., Magee, Andrew, Haruhiru, Alick, and Malsale, Philip
- Published
- 2022
- Full Text
- View/download PDF
3. Traditional or contemporary weather and climate forecasts: reaching Pacific communities
- Author
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Chambers, Lynda, Lui, Siosinamele, Plotz, Roan, Hiriasia, David, Malsale, Philip, Pulehetoa-Mitiepo, Rossylynn, Natapei, Melinda, Sanau, Noel, Waiwai, Mike, Tahani, Lloyd, Willy, Albert, Finaulahi, Seluvaia, Loloa, Falosita, and Fa’anunu, ‘Ofa
- Published
- 2019
- Full Text
- View/download PDF
4. Historical and future drought impacts in the Pacific islands and atolls
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Iese, Viliamu, Kiem, Anthony S., Mariner, Azarel, Malsale, Philip, Tofaeono, Tile, Kirono, Dewi G.C., Round, Vanessa, Heady, Craig, Tigona, Robson, Veisa, Filipe, Posanau, Kisolel, Aiono, Faapisa, Haruhiru, Alick, Daphne, Arieta, Vainikolo, Vaiola, and Iona, Nikotemo
- Published
- 2021
- Full Text
- View/download PDF
5. Traditional knowledge for climate resilience in the Pacific Islands
- Author
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Nunn, Patrick D., Kumar, Roselyn, Barrowman, Hannah M., Chambers, Lynda, Fifita, Laitia, Gegeo, David, Gomese, Chelcia, McGree, Simon, Rarai, Allan, Cheer, Karen, Esau, Dorothy, Fa'anunu, 'Ofa, Fong, Teddy, Fong‐Lomavatu, Mereia, Geraghty, Paul, Heorake, Tony, Kekeubata, Esau, Korovulavula, Isoa, Kubunavanua, Eferemo, Lui, Siosinamele, MacLaren, David, Malsale, Philip, Nemani, Sipiriano, Plotz, Roan D., Puairana, Gaylyn, Rantes, Jimmy, Singh‐Peterson, Lila, and Waiwai, Mike
- Abstract
Pacific Islands, many relatively remote and small, have been occupied by people for more than 3000 years during which time they experienced climate‐driven environmental changes (both slow and rapid onset) that challenged human survival and led to the evolution of place‐based coping strategies expressed through traditional knowledge (TK). In today's globalized Pacific Islands region, into which western worldviews and global adaptation strategies have made significant inroads, most plans for coping with climate‐changed futures are founded in science‐based understandings of the world that undervalue and sideline TK. Many such plans have proved difficult to implement as a consequence. This paper reviews the nature of extant Pacific TK for coping with climate change, something that includes TK for anticipating climate change (including climate variability and climate extremes) as well as ancillary TK associated with food and water security, traditional ecological knowledge, environmental conservation, and settlement and house construction that represent coping strategies. Much of this TK can be demonstrated as being effective with precedents in other (traditional) contexts and a compelling plausible scientific basis. This study demonstrates that Pacific Islands TK for coping with climate change has value and, especially because of its place‐based nature, should be central to future climate‐change adaptation strategies to enhance their uptake, effectiveness and sustainability. To this end, this paper proposes specific ways forward to optimize the utility of TK and ensure it has a realistic role in sustaining Pacific Island communities into the future. This article is categorized under:Climate, History, Society, Culture > Ideas and KnowledgePaleoclimates and Current Trends > Modern Climate ChangeAssessing Impacts of Climate Change > Observed Impacts of Climate Change Ol Pasifik Aelan, plante oli smol mo oli stap wanwan, oli bin gat man i stap long olgeta blong moa long 3000 yia long wan taem we oli bin go tru long ol jenis long envaeromen long ol aelan ia we klaemet nao i mekem (i tekem ples slo mo kwiktaem) mo hemia i jalenjem laef blong ol man long taem ia mo i mekem se oli statem blong kamap wetem ol fasin blong laef wetem ol jenis ia folem wanem aelan oli stap long hem. Ol fasin ia yumi kolem se “traditional knowledge—TK” long Inglis o tradisinol noledj. Long wol blong tedei long Pasifik Aelan rijen, plante plan blong dil wetem wan fiutja we klaemet jenis i jenisim hem i bes plante long ol save blong saens mo hemia i pusum TK i go long wan saed. Hemia yumi luk from ol tingting blong westen wol mo ol strateji o fasin blong faenem wan solusen blong raon wol adaptesen (olsem wanem blong get yus long hem) i afektem. Plante long ol plan ia i had lelebet blong karemaot from hemia. Pepa ia bae i lukluk long hao Pasifik TK we yumi stap yusum finis i stap dil wetem klaemet jenis, wan samting we i yusum TK long klaemet jenis we bae i kam yet (hemia i minim hao klaemet i stap jenis bigwan mo olsem wanem klaemet i muvmuv i go nogud olgeta) mo tu ol nara TK long saed blong kakae mo wota sikiuriti, tradisonel noledj long saed blong fisikel ples mo ol laef we i stap long hem, konsevesen blong envaeromen, mo setelmen mo konstraksen blong ol haos we i soem hao we yumi stap dil wetem situesen olsem. Plante long ol TK ia yumi save luk se hem i wok gud wetem ol nara (tradisenol) situesen we i stap finis mo luksave mo akseptem tru long ol stadi blong saens. Stadi ia i soemaot se Pasifik Aelan TK i gat valiu long saed blong folem mo dil wetem klaemet jenis, from yumi dil wetem long wanwan aelan, mo hemia i sud kam stamba tingting taem yumi kamap wetem ol solusen blong klaemet‐jenis long fiutja, olsem ia yumi save yusum gud samting we i stap finis, i saksesful mo holem taet i stap. Blong kasem hemia, pepa ia i lukluk long ol invesmen we Pasifik TK we ol i niu mo olgeta we i stap long taem naoia. Pepa ia i putumaot ol stret fasin blong folem i go blong yusum mo mekem sua se i gat wan stret mo tru wok blong hem blong holem taet ol Pasifik Aelan komuniti i go long fiutja. Top left x 2—water‐conserving taro terracing (Fiji). Top center—emmakfor water security (Marshall Islands). Top right – augural clouds resemble the stomach of the buff‐banded rail (Fiji). Center right—Tonga Meteorological Service logo shows lofa talamatangi(frigate bird) whose presence over land indicates cyclone. Bottom right—cyclone house (Vanuatu). Bottom left—traditional bure(Fiji).
- Published
- 2024
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- View/download PDF
6. An updated assessment of trends and variability in total and extreme rainfall in the western Pacific
- Author
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Mcgree, S, Whan, K, Jones, D, Alexander, LV ; https://orcid.org/0000-0002-5635-2457, Imielska, A, Diamond, H, Ene, E, Finaulahi, S, Inape, K, Jacklick, L, Kumar, R, Laurent, V, Malala, H, Malsale, P, Moniz, T, Ngemaes, M, Peltier, A, Porteous, A, Pulehetoa-Mitiepo, R, Seuseu, S, Skilling, E, Tahani, L, Teimitsi, F, Toorua, U, Vaiimene, M, Mcgree, S, Whan, K, Jones, D, Alexander, LV ; https://orcid.org/0000-0002-5635-2457, Imielska, A, Diamond, H, Ene, E, Finaulahi, S, Inape, K, Jacklick, L, Kumar, R, Laurent, V, Malala, H, Malsale, P, Moniz, T, Ngemaes, M, Peltier, A, Porteous, A, Pulehetoa-Mitiepo, R, Seuseu, S, Skilling, E, Tahani, L, Teimitsi, F, Toorua, U, and Vaiimene, M
- Abstract
Rainfall records for 23 countries and territories in the western Pacific have been collated for the purpose of examining trends in total and extreme rainfall since 1951. For some countries this is the first time that their data have been included in this type of analysis and for others the number of stations examined is more than twice that available in the current literature. Station trends in annual total and extreme rainfall for 1961-2011 are spatially heterogeneous and largely not statistically significant. This differs with the results of earlier studies that show spatially coherent trends that tended to reverse in the vicinity of the South Pacific Convergence Zone (SPCZ). We infer that the difference is due to the Interdecadal Pacific Oscillation switching to a negative phase from about 1999, largely reversing earlier rainfall changes. Trend analyses for 1981-2011 show wetter conditions in the West Pacific Monsoon (WPM) region and southwest of the mean SPCZ position. In the tropical North Pacific it has become wetter west of 160°E with the Intertropical Convergence Zone/WPM expanding northwards west of 140°E. Northeast of the SPCZ and in the central tropical Pacific east of about 160°E it has become drier. Our findings for the South Pacific subtropics are consistent with broader trends seen in parts of southern and eastern Australia towards reduced rainfall. The relationship between total and extreme rainfall and Pacific basin sea surface temperatures (SSTs) has been investigated with a focus on the influence of the El Niño-Southern Oscillation (ENSO). We substantiate a strong relationship between ENSO and total rainfall and establish similar relationships for the threshold extreme indices. The percentile-based and absolute extreme indices are influenced by ENSO to a lesser extent and in some cases the influence is marginal. Undoubtedly, larger-scale SST variability is not the only influence on these indices. © 2013 Bureau of Meteorology (Australia). Internati
- Published
- 2014
7. Trends and variability of temperature extremes in the tropical Western Pacific
- Author
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Whan, K, Alexander, LV, Imielska, A, Mcgree, S, Jones, D, Ene, E, Finaulahi, S, Inape, K, Jacklick, L, Kumar, R, Laurent, V, Malala, H, Malsale, P, Pulehetoa-Mitiepo, R, Ngemaes, M, Peltier, A, Porteous, A, Seuseu, S, Skilling, E, Tahani, L, Toorua, U, Vaiimene, M, Whan, K, Alexander, LV, Imielska, A, Mcgree, S, Jones, D, Ene, E, Finaulahi, S, Inape, K, Jacklick, L, Kumar, R, Laurent, V, Malala, H, Malsale, P, Pulehetoa-Mitiepo, R, Ngemaes, M, Peltier, A, Porteous, A, Seuseu, S, Skilling, E, Tahani, L, Toorua, U, and Vaiimene, M
- Abstract
A new high-quality daily and monthly temperature station dataset was prepared for the tropical Western Pacific through a quality control and homogenization process. The homogeneity of 46 temperature stations, collected at a workshop conducted as part of the Pacific-Australia Climate Change Science and Adaptation Planning program, was assessed and the non-climatic step changes were removed. Here we present trends in mean and extreme temperature for the Western Pacific, covering an extended time period and larger geographical area compared with previous analyses. We discuss five main conclusions: (1) There is a significant warming trend in annual mean temperature over the past 50 years (1961-2011), of between 0.05 and 0.34°C per decade. (2) Significant and spatially homogeneous warming trends are evident at the station level over 1961-2011 for the warm and cool extremes of both maximum and minimum temperatures. (3) Sub-regional trends, over the period 1951-2011, are spatially coherent, with the largest warming trends in the hottest day and night of the year and the coolest night of the year. (4) This analysis highlights the role of decadal variability in the number of days exceeding extreme temperature thresholds, with the upper (lower) tails of the distribution warming more (less) in recent decades. (5) We show that strong relationships exist between local and remote sea-surface temperature anomalies and all indices of extreme temperature, particularly with minimum temperature extremes. © 2013 The Authors. International Journal of Climatology published by John Wiley & Sons Ltd on behalf of the Royal Meteorological Society.
- Published
- 2014
8. An updated assessment of trends and variability in total and extreme rainfall in the western Pacific
- Author
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McGree, S., primary, Whan, K., additional, Jones, D., additional, Alexander, L. V., additional, Imielska, A., additional, Diamond, H., additional, Ene, E., additional, Finaulahi, S., additional, Inape, K., additional, Jacklick, L., additional, Kumar, R., additional, Laurent, V., additional, Malala, H., additional, Malsale, P., additional, Moniz, T., additional, Ngemaes, M., additional, Peltier, A., additional, Porteous, A., additional, Pulehetoa‐Mitiepo, R., additional, Seuseu, S., additional, Skilling, E., additional, Tahani, L., additional, Teimitsi, F., additional, Toorua, U., additional, and Vaiimene, M., additional
- Published
- 2013
- Full Text
- View/download PDF
9. Trends and variability of temperature extremes in the tropical Western Pacific
- Author
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Whan, K., primary, Alexander, L. V., additional, Imielska, A., additional, McGree, S., additional, Jones, D., additional, Ene, E., additional, Finaulahi, S., additional, Inape, K., additional, Jacklick, L., additional, Kumar, R., additional, Laurent, V., additional, Malala, H., additional, Malsale, P., additional, Pulehetoa‐Mitiepo, R., additional, Ngemaes, M., additional, Peltier, A., additional, Porteous, A., additional, Seuseu, S., additional, Skilling, E., additional, Tahani, L., additional, Toorua, U., additional, and Vaiimene, M., additional
- Published
- 2013
- Full Text
- View/download PDF
10. An updated analysis of homogeneous temperature data at Pacific Island stations
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Jones, D, primary, Collins, D, additional, McGree, S, additional, Trewin, B, additional, Skilling, E, additional, Diamond, H, additional, Fa'anunu, O, additional, Hiriasia, D, additional, Hugony, S, additional, Hutchinson, R, additional, Inape, K, additional, Jacklick, L, additional, Malsale, P, additional, Moniz, T, additional, Ngemaes, M, additional, Porteous, A, additional, Seuseu, S, additional, Tahani, L, additional, Teimitsi, F, additional, Toorua, U, additional, Vaiimene, M, additional, Vuniyayawa, V, additional, and Vavae, H, additional
- Published
- 2013
- Full Text
- View/download PDF
11. An updated assessment of trends and variability in total and extreme rainfall in the western Pacific.
- Author
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McGree, S., Whan, K., Jones, D., Alexander, L. V., Imielska, A., Diamond, H., Ene, E., Finaulahi, S., Inape, K., Jacklick, L., Kumar, R., Laurent, V., Malala, H., Malsale, P., Moniz, T., Ngemaes, M., Peltier, A., Porteous, A., Pulehetoa‐Mitiepo, R., and Seuseu, S.
- Subjects
RAINFALL ,DATA analysis ,CONVERGENCE (Meteorology) ,METEOROLOGICAL precipitation measurement ,PRECIPITATION variability ,PACIFIC Ocean currents - Abstract
Rainfall records for 23 countries and territories in the western Pacific have been collated for the purpose of examining trends in total and extreme rainfall since 1951. For some countries this is the first time that their data have been included in this type of analysis and for others the number of stations examined is more than twice that available in the current literature. Station trends in annual total and extreme rainfall for 1961-2011 are spatially heterogeneous and largely not statistically significant. This differs with the results of earlier studies that show spatially coherent trends that tended to reverse in the vicinity of the South Pacific Convergence Zone (SPCZ). We infer that the difference is due to the Interdecadal Pacific Oscillation switching to a negative phase from about 1999, largely reversing earlier rainfall changes. Trend analyses for 1981-2011 show wetter conditions in the West Pacific Monsoon (WPM) region and southwest of the mean SPCZ position. In the tropical North Pacific it has become wetter west of 160°E with the Intertropical Convergence Zone/WPM expanding northwards west of 140°E. Northeast of the SPCZ and in the central tropical Pacific east of about 160°E it has become drier. Our findings for the South Pacific subtropics are consistent with broader trends seen in parts of southern and eastern Australia towards reduced rainfall. The relationship between total and extreme rainfall and Pacific basin sea surface temperatures (SSTs) has been investigated with a focus on the influence of the El Niño-Southern Oscillation (ENSO). We substantiate a strong relationship between ENSO and total rainfall and establish similar relationships for the threshold extreme indices. The percentile-based and absolute extreme indices are influenced by ENSO to a lesser extent and in some cases the influence is marginal. Undoubtedly, larger-scale SST variability is not the only influence on these indices. [ABSTRACT FROM AUTHOR]
- Published
- 2014
- Full Text
- View/download PDF
12. Trends and variability of temperature extremes in the tropical Western Pacific.
- Author
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Whan, K., Alexander, L. V., Imielska, A., McGree, S., Jones, D., Ene, E., Finaulahi, S., Inape, K., Jacklick, L., Kumar, R., Laurent, V., Malala, H., Malsale, P., Pulehetoa‐Mitiepo, R., Ngemaes, M., Peltier, A., Porteous, A., Seuseu, S., Skilling, E., and Tahani, L.
- Subjects
PRECIPITATION variability ,CLIMATE change ,TEMPERATURE ,METEOROLOGY ,BIOLOGICAL adaptation ,GLOBAL warming - Abstract
A new high-quality daily and monthly temperature station dataset was prepared for the tropical Western Pacific through a quality control and homogenization process. The homogeneity of 46 temperature stations, collected at a workshop conducted as part of the Pacific-Australia Climate Change Science and Adaptation Planning program, was assessed and the non-climatic step changes were removed. Here we present trends in mean and extreme temperature for the Western Pacific, covering an extended time period and larger geographical area compared with previous analyses. We discuss five main conclusions: (1) There is a significant warming trend in annual mean temperature over the past 50 years (1961-2011), of between 0.05 and 0.34 °C per decade. (2) Significant and spatially homogeneous warming trends are evident at the station level over 1961-2011 for the warm and cool extremes of both maximum and minimum temperatures. (3) Sub-regional trends, over the period 1951-2011, are spatially coherent, with the largest warming trends in the hottest day and night of the year and the coolest night of the year. (4) This analysis highlights the role of decadal variability in the number of days exceeding extreme temperature thresholds, with the upper (lower) tails of the distribution warming more (less) in recent decades. (5) We show that strong relationships exist between local and remote sea-surface temperature anomalies and all indices of extreme temperature, particularly with minimum temperature extremes. [ABSTRACT FROM AUTHOR]
- Published
- 2014
- Full Text
- View/download PDF
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