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Does elevation dependent warming exist in high mountain Asia

Bibliographic Data

ID15546124
AuthorsBaofu Li (0000-0001-6986-135X, Qufu Normal University, corresponding author), Yaning Chen (0000-0001-6742-1641, Chinese Academy of Sciences), Xun Shi (0000-0002-7169-5175, Dartmouth College)
Year2020
Volume15
Issue2
Pages024012-024012
Publication date2020-01-20
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ab6d7f
OpenAlexW3000986364
LanguageEN
Citations received4
References cited57

A majority of studies suggest that elevation dependent warming (EDW) has been verified in mountainous areas. However, there is some controversy about the EDW of high mountain Asia (HMA). Based on the analysis of the data from 128 meteorological stations in the entire region for 1961–2017, we found that there was no EDW in HMA on the time scale of 1961–2017 and the spatial scale of the altitude of 3500–5000 m. The EDW in HMA is the most obvious during the period of 1998–2012. In general, after 1980, there was EDW in the altitude of 2500–5000 m. The Southeastern Tibetan Plateau always has EDW phenomenon for most of the time scales while other areas only have EDW at certain periods. Therefore, we consider that the rate of warming is higher only in specific mountain areas and time scales

Altitude (triangle · Cartography · Climatology · Effects of high altitude on humans · Elevation (ballistics · Geography · Meteorology · Physical geography · Plateau (mathematics · Scale (ratio · Climate change and permafrost · Climate variability and models · Cryospheric studies and observations · Environmental Science · Geology

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Unique citing works4
Citations per year1
Citation span2022 - 2024 (3)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 4

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