The 30 participants represented a crosscut
of glaciological and ocean modelers spanning the international community.
Reanalysis of long - term series
of glaciological and geodetic mass balance for 10 Norwegian glaciers, The Cryosphere, 10, 535 - 552, doi: 10.5194 / tc -10-535-2016.
A key area
of glaciological study in recent years is ice sheet mass balance.
(Much
of the glaciological literature on termination of large ice ages requires ice - sheet growth past a threshold size.)
Jean - Louis Tison is a Glaciologist, and the Co-director
of the Glaciological Laboratory of the Department of Earth and Environmental Sciences (Université Libre de Bruxelles).
Not exact matches
The causes
of the age differences at MIS 5 were proposed to occur from (i) an overestimation
of the surface mass balance at around MIS 5d - 6 in the
glaciological model, and (ii) an error in one
of the age constraints by ~ 3 kyr at MIS 5b.
According to the study, published in the International
Glaciological Society's Journal
of Glaciology, the first decade
of the twenty - first century witnessed a «historically unprecedented» rate
of glacial ice melt.
According to a new study, published in the International
Glaciological Society's Journal
of Glaciology, the first decade
of the twenty - first century witnessed a «historically unprecedented» rate
of glacial ice melt.
Bentley, C.R., The Ross Ice Shelf Geophysical and
Glaciological Survey (RIGGS): Introduction and summary
of measurements performed, Antarctic Research Series, American Geophysical Union, Vol.
Jenkins A, Vaughan DG, Jacobs SS, Hellmer HH, Keys HJR (1997)
Glaciological and oceanographic evidence
of high melt rates beneath Pine Island Glacier, West Antarctica.
Sedimentary history
of the Ross Embayment: a unified hypothesis from a
glaciological perspective.
Bindschadler, Robert Robert Bindschadler is Chief Scientist
of the Laboratory for Hydrospheric and Biospheric Processes at NASA Goddard Space Flight Center, USA, a Senior Fellow
of NASA Goddard, an AGU Fellow and past President
of the International
Glaciological Society.
Frank Pattyn is a Glaciologist and Ice Sheet Modeler at the
Glaciological Laboratory
of the Department
of Earth and Environmental Sciences (Université Libre de Bruxelles).
«Simply put, the shape
of the ice sheet and the contact with the ocean makes it likely that these areas respond more pronouncedly to changes in climate boundary conditions — be they atmospheric, oceanic or
glaciological.»
Your post discusses the proposed correction to the Times Atlas that has resulted from the actions
of the international glaciological research community — which you correctly applaud and hold up as a model for all scientists — «Of course, many scientists can do more, and we encourage all of our colleagues to speak publically about their research and, as the international glaciological research community did in this case, to try to correct misconceptions.&raqu
of the international
glaciological research community — which you correctly applaud and hold up as a model for all scientists — «
Of course, many scientists can do more, and we encourage all of our colleagues to speak publically about their research and, as the international glaciological research community did in this case, to try to correct misconceptions.&raqu
Of course, many scientists can do more, and we encourage all
of our colleagues to speak publically about their research and, as the international glaciological research community did in this case, to try to correct misconceptions.&raqu
of our colleagues to speak publically about their research and, as the international
glaciological research community did in this case, to try to correct misconceptions.»
Of course, it's the international
glaciological research community that has the most relevant expertise.
Pfeffer's «back -
of - the - envelope» calculations are quite compelling (as presented at the Midwest
Glaciological Meeting in Burlington, VT last month).
«Alaskan and immediately adjacent Canadian glaciers supply one
of the largest measured
glaciological contributions to global sea level rise (~ 0.14 mm yr - 1, equivalent to new estimates from Greenland).
The
glaciological community has for decades harbored the widespread belief that the thermal evolution
of the ice sheet, and the effect
of this evolution on ice flow, are central in the ice - age cycling (not all communities agree, but there is plenty
of literature on this from the land - ice crowd), so use
of a temperature - independent rheology for the ice leaves out one favored explanation for termination
of extensive glaciation.
A structural
glaciological analysis
of the 2002 Larsen B ice shelf collapse.
The US CLIVAR Greenland Ice Sheet - Ocean Interactions Working Group was formed to foster and promote interaction between the diverse oceanographic,
glaciological, atmospheric and climate communities, including modelers and field and data scientists within each community, interested in glacier / ocean interactions around Greenland, to advance understanding
of the process and ultimately improve its representation in climate models.
The WGMS reference glaciers have more than 30 years
of ongoing
glaciological mass balance measurements.
The
glaciological threesome report their findings in the journal, The Cryosphere as - Elevation and elevation change
of Greenland and Antarctica derived from CryoSat - 2.
Nozomu Takeuchi, professor
of earth sciences at Chiba University in Japan, said the new research highlights the importance
of accounting for biological processes in the cryosphere, and believes the study will have an impact on
glaciological research
of the Greenland ice sheet.
These geographic separations are made according the
glaciological basins
of Vaughan et al. (1999), which are delineated on a 1 ° × 1 ° mask as described by Monaghan et al. (2006).
WA also excludes the
glaciological basins
of the Peninsula.
«A combination
of geophysical, biological and
glaciological information supports the idea
of a 2,600 year solar cycle» (J.R. Bray.
A deglacial model for Antarctica: geological constraints and
glaciological modelling as a basis for a new model
of Antarctic glacial isostatic adjustment.
The reference glaciers have more than 30 years
of ongoing
glaciological mass - balance measurements.