Spatiotemporal Variations in the Air Freezing and Thawing Index Over the Mongolian Plateau From 1901 to 2019

The Mongolian Plateau is located in the permafrost transitional zone between high-altitudinal and high-latitudinal permafrost regions in the Northern Hemisphere. Current knowledge of the thermal state and changes in the permafrost on the Mongolian Plateau is limited. This study adopted an improved c...

Full description

Bibliographic Details
Published in:Frontiers in Environmental Science
Main Authors: Xin Ma, Tonghua Wu, Xiaofan Zhu, Peiqing Lou, Dong Wang, Saruulzaya Adiya, Dashtseren Avirmed, Battogtokh Dorjgotov, Jie Chen, Chengpeng Shang, Amin Wen, Yune La, Xianhua Wei, Ren Li
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2022
Subjects:
freezing and thawing index
permafrost
CRU
Mongolian plateau
change-point
Environmental sciences
GE1-350
Kendall
Online Access:https://doi.org/10.3389/fenvs.2022.875450
https://doaj.org/article/2de52b5e3a284970b94bcf85da08e471
Description
Summary:The Mongolian Plateau is located in the permafrost transitional zone between high-altitudinal and high-latitudinal permafrost regions in the Northern Hemisphere. Current knowledge of the thermal state and changes in the permafrost on the Mongolian Plateau is limited. This study adopted an improved calculation method of the Mongolian Plateau air freezing and thawing index using the monthly air temperature reanalysis dataset from the Climate Research Unit (CRU). The spatial and temporal variation characteristics from 1901 to 2019 were further assessed by the Mann–Kendall (M–K) test and spatial interpolation methods. The results indicate that the spatial distributions of the freezing and thawing index show clear latitudinal zonality. Over the study period, the air freezing index decreased by 4.1°C·d/yr, and the air thawing index increased by 2.3°C·d/yr. The change point in the air thawing index appeared in 1995 (p < 0.05) based on the M–K method, in contrast to the so-called hiatus in global warming. Our results reveal rapid warming on the Mongolian Plateau, especially in the permafrost region, and are useful for studying permafrost changes on the Mongolian Plateau.

Similar Items