322 results on '"Spagnolo, Matteo"'
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52. Glacier monitoring using real-aperture 94 GHz radar
53. Chapter 40 - The Italian Mountains: glacial landforms from the Bølling–Allerød Interstadial (14.6–12.9 ka)
54. Chapter 23 - The Italian Mountains: glacial landforms during deglaciation (18.9–14.6 ka)
55. Chapter 58 - The Italian Mountains: Glacial landforms from the Younger Dryas Stadial (12.9–11.7 ka)
56. New insights into the Last Glacial Maximum in the Maritime Alps from paleoglacier reconstructions and 10Be surface exposure dating
57. Spatial organization of drumlins
58. New insights into the last glacial cycle in the south-eastern European Alps from the glacial geomorphological record of the Monte Cavallo (NE Italy)
59. Volcanically-triggered changes in glacier surface velocity
60. Millimetre-wave radar observations of glacier calving at Hansbreen (Svalbard) correlated with TLS, time-lapse camera images and seismic records
61. Supplementary material to "Multitemporal glacier inventory revealing four decades of glacier changes in the Ladakh region"
62. The instability theory of drumlin formation and its explanation of their varied composition and internal structure
63. Chapter 42 - The Italian mountains: glacial landforms prior to the Last Glacial Maximum
64. Chapter 61 - The Italian mountains: glacial landforms from the Last Glacial Maximum
65. Chapter 18 - The Italian Peninsula
66. Rapid Sediment Re-Deposition May Limit Carbon Release during Catastrophic Thermokarst Lake Drainage
67. Testing the Area-Altitude Balance Ratio (AABR) and Accumulation Area Ratio (AAR) methods of calculating glacier equilibrium-line altitude
68. A New Approach for the Study of the Coast Indentation Index
69. The composition and internal structure of drumlins: Complexity, commonality, and implications for a unifying theory of their formation
70. Testing the area–altitude balance ratio (AABR) and accumulation–area ratio (AAR) methods of calculating glacier equilibrium-line altitudes
71. The planar shape of drumlins
72. Assessing the Use of Optical Satellite Images to Detect Volcanic Impacts on Glacier Surface Morphology
73. The (mis)conception of average Quaternary conditions
74. Cool deltas: Sedimentological, geomorphological and geophysical characterization of ice‐contact deltas and implications for their reservoir properties (Salpausselkä, Finland)
75. Size and shape characteristics of drumlins, derived from a large sample, and associated scaling laws
76. Size, shape and spatial arrangement of mega-scale glacial lineations from a large and diverse dataset
77. Reconstructing LGM paleoglaciers and their ELAs along the southern fringe of the Eastern European Alps
78. Geomorphologically-controlled seismic signals at Mount St. Helens volcano
79. Using glaciers to identify, monitor, and predict volcanic activity
80. Testing the area–altitude balance ratio (AABR) and accumulation–area ratio (AAR) methods of calculating glacier equilibrium-line altitudes.
81. Glaciations on Ophiolite Terrain in the North Pindus Mountains, Greece: New Geomorphological Insights and Preliminary 36cl Exposure Dating
82. Atmospheric circulation over Europe during the Younger Dryas
83. Main findings: Remotely sensed evidence of volcanic impacts on glaciers
84. Diverse landscapes beneath Pine Island Glacier influence ice flow
85. The (mis)conception of average Quaternary conditions.
86. The topography of drumlins; assessing their long profile shape
87. Observing the cryosphere with millimetre wave radar: The case study of Rhône Glacier
88. Geomorphological controls on seismic recordings in volcanic areas
89. Estimating the style and duration of former glaciation in the mountains of Britain and Ireland
90. The (mis)conception of an average Quaternary equilibrium line altitude
91. Analysing palaeo cirque glacier equilibrium line altitudes as indicators of palaeoclimate across Scandinavia
92. Ice-contact deltas investigation using ground penetrating radar (GPR), sedimentology, electrical resistivity tomography (ERT) and , Salpausselka I and II near Lahti, Finland
93. Using glaciers to identify, monitor, and predict volcanic activity
94. reviewer comments
95. Glaciology in Aberdeen
96. Temperatures recorded by cosmogenic noble gases since the last glacial maximum in the Maritime Alps
97. The effects of late Alpine tectonics in the morphology of the Argentera Massif (Western Alps, Italy–France)
98. Extensive marine-terminating ice sheets in Europe from 2.5 million years ago
99. Using the size and position of drumlins to understand how they grow, interact and evolve
100. Factors controlling alpine glaciations in the Sierra Baguales Mountain Range of southern Patagonia (50° S), inferred from the morphometric analysis of glacial cirques
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