| Registros del 1 al 10 de 392 encontrados |
1.- A 300-YEAR HISTORY OF FLOODING IN AN ANDEAN MOUNTAIN RIVER SYSTEM; THE RIO ALIZOS, SOUTHERN BOLIVIA
A.A. BALKEMA PUBLISHERS;; NLD; NETHERLANDS, 2001
RIVER BASIN SEDIMENT SYSTEMS; ARCHIVES OF ENVIRONMENTAL CHANGE
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2.- A comparison of the suspended and dissolved matter dynamics of two large inter-tropical rivers draining into the Atlantic Ocean; the Congo and the Orinoco
Wiley-Blackwell; New York, NY; USA; United States, 2013
The hydrology of large rivers
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3.- A fifty year record of winter glacier melt events in southern Chile, 38 degrees -42 degrees S
Institute of Physics and IOP Publishing; Bristol; GBR; United Kingdom, 2012
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4.- A GIS tool for modelling annual diffuse infiltration on a plot scale
Elsevier; Amsterdam; NLD; Netherlands, 2013
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5.- A METHOD FOR DROUGHT MONITORING
EUROPEAN GEOPHYSICAL SOCIETY; KATHLENBURG-LINDAU; DEU; FEDERAL REPUBLIC OF GERMANY, 1998
23RD GENERAL ASSEMBLY OF THE EUROPEAN GEOPHYSICAL SOCIETY; HYDROLOGY, OCEANS & ATMOSPHERE
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6.- A potential pollen proxy for ENSO derived from the Sajama ice core
American Geophysical Union; Washington, DC; USA; United States, 2007
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7.- A promising location in Patagonia for paleoclimate and paleoenvironmental reconstructions revealed by a shallow firn core from Monte San Valentin (northern Patagonia Icefield, Chile)
American Geophysical Union; Washington, DC; USA; United States, 2008
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8.- A shift in the spatial pattern of Iberian droughts during the 17th century
Copernicus; Katlenburg-Lindau; III; International, 2010
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9.- A SPECTRAL STUDY OF LONG-TERM WATER HEAD FLUCTUATIONS IN A MEDITERRANEAN DETRITIC AQUIFER
[INTERNATIONAL GEOLOGICAL CONGRESS]; [LOCATION VARIES]; III; INTERNATIONAL, 2004
ITALIA 2004; 32ND INTERNATIONAL GEOLOGICAL CONGRESS; ABSTRACTS
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10.- A VARIABILIDADE DA PRECIPITAÇAO NA PENINSULA IBERICA: A ANALISE DAS ESTRUTURAS ESPACIO-TEMPORAIS DAS OSCILAÇOES MAIS SIGNIFICATIVAS
UNIVERSIDAD POLITECNICA DE VALENCIA; VALENCIA; ESP, 2003
3ª ASAMBLEA HISPANO-PORTUGUESA DE GEODESIA Y GEOFISICA.. PROCEEDINGS. TOMO II
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