Observational Constraint on the Contribution of Surface Albedo Feedback to the Amplified Tibetan Plateau Surface Warming-Reference-Cited by-同舟云学术

Observational Constraint on the Contribution of Surface Albedo Feedback to the Amplified Tibetan Plateau Surface Warming

Published:2022-07-06 Issue:13 Volume:127 Page:
ISSN:2169-897X
Container-title:Journal of Geophysical Research: Atmospheres
language:en
Short-container-title:JGR Atmospheres

Author:

Chen Yan¹,Ji Duoying¹^ORCID,Moore John C.¹²³^ORCID,Hu Jiangling¹,He Yanyi⁴

Affiliation:

1. College of Global Change and Earth System Science Beijing Normal University Beijing China

2. Arctic Centre University of Lapland Rovaniemi Finland

3. CAS Center for Excellence in Tibetan Plateau Earth Sciences Beijing China

4. Department of Earth System Science Ministry of Education Key Laboratory for Earth System Modeling Institute for Global Change Studies Tsinghua University Beijing China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JD036085

Reference122 articles.

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2. Satellite and Ground Observations of Snow Cover in Tibet during 2001–2015

3. Beijing Normal University/China. (2013).GLASS: Long‐term GLASS Albedo product[Dataset].Research Data Archive at the National Earth System Science Data Center National Science & Technology Infrastructure of China.https://doi.org/10.12041/geodata.GLASS_Albedo_avhrr.ver1.db

4. Multiscale Changes in Snow Over the Tibetan Plateau During 1980–2018 Represented by Reanalysis Data Sets and Satellite Observations

5. Evaluation of the Arctic surface radiation budget in CMIP5 models

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