dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel Estimation of lake water storage change and its linkage to increased mass on the Tibetan Plateau
VerfasserIn Liping Zhu, Baojin Qiao
Konferenz EGU General Assembly 2017
Medientyp Artikel
Sprache en
Digitales Dokument PDF
Erschienen In: GRA - Volume 19 (2017)
Datensatznummer 250144924
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2017-8805.pdf
 
Zusammenfassung
In this study, we estimated water storage change of 282 lakes (> 10 km2) by an empirical equation based on Shuttle Radar Topography Mission (SRTM) DEM and Landsat images in the endorheic basin of inner Tibetan Plateau (ITP). Lakes water storage had increased by 107.5 Gt (8.27 Gt/y) from 2000 to 2013, 89.4 % of increased water storage was mainly concentrated in four regions and 126 large lakes (> 50 km2) occupied 90.6 % of total water storage change. Mass increased rate of ITP was 4.38 Gt/y derived from Gravity Recovery and Climate Experiment (GRACE) satellite data during 2003-2009, which could explain 53 % of lake expansion. A little contribution to lake from permafrost degradation based on Active-layer depth (ALD) model. Increased glacial meltwater with rising temperature, which didn’t increase mass of ITP, made an equivalent contribution to lake expansion with precipitation and evaporation.