about
Actively evolving subglacial conduits and eskers initiate ice shelf channels at an Antarctic grounding line.Getting around Antarctica: new high-resolution mappings of the grounded and freely-floating boundaries of the Antarctic ice sheet created for the International Polar YearMeltwater produced by wind–albedo interaction stored in an East Antarctic ice shelfHigh variability of climate and surface mass balance induced by Antarctic ice risesConstraining variable density of ice shelves using wide-angle radar measurementsDynamic influence of pinning points on marine ice-sheet stability: a numerical study in Dronning Maud Land, East AntarcticaAntarctic ice rises and rumples: Their properties and significance for ice-sheet dynamics and evolutionDetecting high spatial variability of ice shelf basal mass balance, Roi Baudouin Ice Shelf, AntarcticaThe control of an uncharted pinning point on the flow of an Antarctic ice shelfIce core evidence for a 20th century increase in surface mass balance in coastal Dronning Maud Land, East AntarcticaPotential mechanisms for anisotropy in ice-penetrating radar dataTemporally stable surface mass balance asymmetry across an ice rise derived from radar internal reflection horizons through inverse modelingEvolution of Derwael Ice Rise in Dronning Maud Land, Antarctica, over the last millennia
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P50
description
German geophysicist
@en
deutscher Geophysiker
@de
geofysicus
@nl
name
R Drews
@nl
Reinhard Drews
@de
Reinhard Drews
@en
Reinhard Drews
@es
type
label
R Drews
@nl
Reinhard Drews
@de
Reinhard Drews
@en
Reinhard Drews
@es
altLabel
R Drews
@en
prefLabel
R Drews
@nl
Reinhard Drews
@de
Reinhard Drews
@en
Reinhard Drews
@es
P227
P106
P21
P214
5081149198298874940003
P227
1177534037
P31
P496
0000-0002-2328-294X
P7859
viaf-5081149198298874940003