Article
Version 1
Preserved in Portico This version is not peer-reviewed
Snow Cover on the Tibetan Plateau and Topographic Controls
Version 1
: Received: 3 July 2023 / Approved: 3 July 2023 / Online: 3 July 2023 (09:52:34 CEST)
A peer-reviewed article of this Preprint also exists.
Chu, D.; Liu, L.; Wang, Z. Snow Cover on the Tibetan Plateau and Topographic Controls. Remote Sens. 2023, 15, 4044. Chu, D.; Liu, L.; Wang, Z. Snow Cover on the Tibetan Plateau and Topographic Controls. Remote Sens. 2023, 15, 4044.
Abstract
Snow cover plays a critical role in the global energy and water cycles. Snow cover on the Tibetan Plateau (TP) provides vital water sources in western China and Himalayan regions in addition to its weather and climate significance. The massive high mountain topography of the TP is main conditions for the presence and persistence of snow cover on the plateau at the mid-low latitudes of the Northern Hemisphere (NH). However, how mountain topography controls snow cover distribution on the TP is largely remain unclear and the relationship is not well quantified. Here, the spatial distribution of snow cover and topographic controls on snow cover on the TP are examined based on snow cover frequency (SCF) derived from MODIS snow cover product (MOD10A2 v5) and digital elevation model (DEM). The results show that snow cover on the TP is spatially unevenly distributed and is characterized by rich snow and high SCF on the interior and surrounding high mountain ranges, and less snow and low SCF in inland basins and river valleys. Snow cover on the TP presents elevation dependence with the higher the altitude, the higher the SCF, the longer the snow cover duration and the more stable the intra-annual variation. Annual mean SCF below 3000 m above sea level (masl) is less than 4% and it reaches 77% above 6000 masl. The intra-annual snow cover variation below 4000 masl features a unimodal distribution, while above 4000 masl it presents a bimodal distribution. The mean minimum SCF below 6000 masl occurs in summer, while above 6000 masl it occurs in winter. Because of differences in solar radiation and water vapor sources, mean SCF generally increases with mountain slopes and it is the highest on the north-facing aspect, whereas the lowest is observed on the south-facing aspect.
Keywords
MODIS snow cover; SRTM DEM; topographic elements, Tibetan Plateau
Subject
Environmental and Earth Sciences, Remote Sensing
Copyright: This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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