Instituto Geológico y Minero de España

LogoSistema de información documental - SID

 

 

 

Resultados de la consulta :
Instituto Geológico y Minero de España
 Registros del al 8 de 8 encontrados

1.-  Atmospheric warming at a high-elevation tropical site revealed by englacial temperatures at Illimani, Bolivia (6340 m above sea level, 6 degrees S, 67 degrees W)
American Geophysical Union; Washington, DC; USA; United States, 2010
Ver registro

2.-  Climate change and tropical Andean glaciers; past, present and future
Elsevier; Amsterdam; NLD; Netherlands, 2008
Ver registro

3.-  Distributed snow and ground models over a 67% glacierized basin in Bolivia (Zongo Glacier, tropical Andes) to study melting processes and to simulate water discharge
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2008
European Geosciences Union general assembly 2008
Ver registro

4.-  Establishing an empirical relationship between bare soil albedo and surface soil moisture of the Zongo Glacier (Bolivia) from in-situ measurements
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Federal R, 2008
European Geosciences Union general assembly 2008
Ver registro

5.-  Irregular retreat of tropical glaciers during the Holocene
Mineralogical Society; London; GBR; United Kingdom, 2011
Goldschmidt 2011 abstract volume
Ver registro

6.-  Mass balance of Glaciar Zongo, Bolivia, between 1956 and 2006, using glaciological, hydrological and geodetic methods
International Glaciological Society; Cambridge; GBR; United Kingdom, 2009
Mass-balance measurements and modelling
Ver registro

7.-  Measured and modelled sublimation on the tropical Glaciar Artesonraju, Peru
Copernicus on behalf of the European Geosciences Union; Katlenburg-Lindau; III; International, 2009
Ver registro

8.-  Sensitivity of bare soil albedo to surface soil moisture on the moraine of the Zongo Glacier (Bolivia)
American Geophysical Union; Washington, DC; USA; United States, 2009
Ver registro


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