Multi-Proxy, Multi-Season Streamflow Reconstruction with Mass Balance Adjustment
Despite having offered important hydroclimatic insights, streamflow reconstructions still see limited use in water resources operations, because annual reconstructions are not suitable for decisions at finer time scales. The few attempts toward sub-annual reconstructions have relied on statistical disaggregation, which uses none or little proxy ...
Hung Nguyen +3 more
+6 more sources
A New 200‐Year Spatial Reconstruction of West Antarctic Surface Mass Balance [PDF]
AbstractHigh‐spatial resolution surface mass balance (SMB) over the West Antarctic Ice Sheet (WAIS) spanning 1800–2010 is reconstructed by means of ice core records combined with the outputs of the European Centre for Medium‐Range Weather Forecasts “Interim” reanalysis (ERA‐Interim) and the latest polar version of the Regional Atmospheric Climate Model
Yetang Wang +5 more
openalex +5 more sources
A century reconstruction of the mass balance of Glacier de Sarennes, French Alps [PDF]
AbstractThe 50 year time series of mass balance on Glacier de Sarennes is one of the longest in the French Alps, and so is often used as a reference for glacier variations in the French Alps. Meteorological data can be used to extend the series backwards in time. Martin (1978) proposed such a reconstruction for the 1882–1977 period.
Olivier Torinesi +2 more
openalex +3 more sources
A reconstruction of annual mass balances of Austria’s glaciers from 1969 to 1998 [PDF]
AbstractAnnual glacier mass balances are reconstructed for 96% of the Austrian glacier-covered area (451 of 470 km2) between 1969 and 1998. The volume change derived from two complete glacier inventories (1969 and 1998) serves as the boundary condition that is aimed to be reproduced.
Jakob Abermann +2 more
+4 more sources
Disaggregating geodetic glacier mass balance to annual scale using remote-sensing proxies
Decadal-scale, high-resolution geodetic measurements of glacier thinning have transformed our understanding of glacier response to climate change. Annual glacier mass balance can be estimated using remote-sensing proxies like snow-line altitude.
Argha Banerjee +2 more
doaj +1 more source
Reduced accuracy in dendroglaciological mass balance reconstruction of Storglaciären since the 1980s [PDF]
Recent studies have raised concerns regarding the reconstruction of glacier mass balance using tree-ring data. The method relies on a stable relationship between both variables and summer (June–August) or melt season (May–September) temperature. However, with recent anthropogenic climate change the stability of this relationship is challenged by both,
Niklas Werner +3 more
openalex +3 more sources
Reconstruction of the 1979–2006 Greenland ice sheet surface mass balance using the regional climate model MAR [PDF]
Results from a 28-year simulation (1979–2006) over the Greenland ice sheet (GrIS) reveal an increase of solid precipitation (+0.4±2.5 km3 yr−2) and run-off (+7.9±3.3 km3 yr−2) of surface meltwater.
X. Fettweis
doaj +1 more source
Greenland Ice Sheet Mass Balance Reconstruction. Part I: Net Snow Accumulation (1600–2009) [PDF]
Abstract Ice core data are combined with Regional Atmospheric Climate Model version 2 (RACMO2) output (1958–2010) to develop a reconstruction of Greenland ice sheet net snow accumulation rate, Ât(G), spanning the years 1600–2009. Regression parameters from regional climate model (RCM) output regressed on 86 ice cores are used with ...
Jason E. Box +10 more
openalex +5 more sources
Reconstruction of Glacier Mass Balances and Climate Changes in the Kamchatka Peninsula.
More than 400 glaciers exist in the mountains of Kamchatka Peninsula and they constitute the southern boundary of present-day glacierization along the eastern coast of the Eurasian continent. The mass balances of the glaciers are characterized by decadal and interdecadal oscillations, and they are closely related to those observed in the glaciers of ...
Takayuki Shiraiwa, Satoru Yamaguchi
openalex +3 more sources
Greenland Ice Sheet Mass Balance Reconstruction. Part II: Surface Mass Balance (1840–2010)*
Abstract Meteorological station records, ice cores, and regional climate model output are combined to develop a continuous 171-yr (1840–2010) reconstruction of Greenland ice sheet climatic surface mass balance (Bclim) and its subcomponents including near-surface air temperature (SAT) since the end of the Little Ice Age.
Jason E. Box, William Colgan
openaire +2 more sources

