about
Postglacial response of Arctic Ocean gas hydrates to climatic amelioration.Massive blow-out craters formed by hydrate-controlled methane expulsion from the Arctic seafloor.Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming.Regulation of ice stream flow through subglacial formation of gas hydratesThe configuration, sensitivity and rapid retreat of the Late Weichselian Icelandic ice sheetThe last Welsh Ice Cap: Part 1 - Modelling its evolution, sensitivity and associated climateThe last Welsh Ice Cap: Part 2 - Dynamics of a topographically controlled icecapDynamic cycles, ice streams and their impact on the extent, chronology and deglaciation of the British–Irish ice sheetDeglaciation of the Eurasian ice sheet complexAmplified melt and flow of the Greenland ice sheet driven by late-summer cyclonic rainfallAutomated mapping of glacial overdeepenings beneath contemporary ice sheets: Approaches and potential applicationsThe build-up, configuration, and dynamical sensitivity of the Eurasian ice-sheet complex to Late Weichselian climatic and oceanic forcingGeophysical constraints on the dynamics and retreat of the Barents Sea ice sheet as a paleobenchmark for models of marine ice sheet deglaciationEvaluation of a numerical model of the British-Irish ice sheet using relative sea-level data: implications for the interpretation of trimline observations
P50
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P50
description
onderzoeker
@nl
researcher, ORCID id # 0000-0001-9670-611X
@en
name
Henry Patton
@ast
Henry Patton
@en
Henry Patton
@es
Henry Patton
@nl
type
label
Henry Patton
@ast
Henry Patton
@en
Henry Patton
@es
Henry Patton
@nl
prefLabel
Henry Patton
@ast
Henry Patton
@en
Henry Patton
@es
Henry Patton
@nl
P106
P1153
26031683300
P31
P496
0000-0001-9670-611X