Mechanism of non-appearance of hiatus in Tibetan Plateau

Abstract In the recent decade, hiatus is the hottest issue in the community of climate change. As the area of great importance, the Tibetan Plateau (TP), however, did not appear to have any warming stoppage in the hiatus period. In fact, the TP showed a continuous warming in the recent decade. To ex...

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Autores principales: Jieru Ma, Xiaodan Guan, Ruixia Guo, Zewen Gan, Yongkun Xie
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Lenguaje:EN
Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/9cd0332315794204978dbcfbaafad541
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spelling oai:doaj.org-article:9cd0332315794204978dbcfbaafad5412021-12-02T15:05:09ZMechanism of non-appearance of hiatus in Tibetan Plateau10.1038/s41598-017-04615-72045-2322https://doaj.org/article/9cd0332315794204978dbcfbaafad5412017-06-01T00:00:00Zhttps://doi.org/10.1038/s41598-017-04615-7https://doaj.org/toc/2045-2322Abstract In the recent decade, hiatus is the hottest issue in the community of climate change. As the area of great importance, the Tibetan Plateau (TP), however, did not appear to have any warming stoppage in the hiatus period. In fact, the TP showed a continuous warming in the recent decade. To explore why the TP did not show hiatus, we divide the surface air temperature into dynamically-induced temperature (DIT) and radiatively-forced temperature (RFT) by applying the dynamical adjustment method. Our results show that DIT displayed a relatively uniform warming background in the TP, with no obvious correlations with dynamic factors. Meanwhile, as the major contribution to warming, the RFT effect over the TP played the dominant role. The warming role is illustrated using the temperature change between perturbed and control simulation responses to CO2 or black carbon (BC) forcing via Community Earth System Model (CESM). It shows that an obvious warming in the TP is induced by the CO2 warming effect, and BC exhibits an amplifying effect on the warming. Therefore, the continuous warming in the TP was a result of uniform DIT warming over a large scale and enhanced RFT warming at a regional scale.Jieru MaXiaodan GuanRuixia GuoZewen GanYongkun XieNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 7, Iss 1, Pp 1-11 (2017)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Jieru Ma
Xiaodan Guan
Ruixia Guo
Zewen Gan
Yongkun Xie
Mechanism of non-appearance of hiatus in Tibetan Plateau
description Abstract In the recent decade, hiatus is the hottest issue in the community of climate change. As the area of great importance, the Tibetan Plateau (TP), however, did not appear to have any warming stoppage in the hiatus period. In fact, the TP showed a continuous warming in the recent decade. To explore why the TP did not show hiatus, we divide the surface air temperature into dynamically-induced temperature (DIT) and radiatively-forced temperature (RFT) by applying the dynamical adjustment method. Our results show that DIT displayed a relatively uniform warming background in the TP, with no obvious correlations with dynamic factors. Meanwhile, as the major contribution to warming, the RFT effect over the TP played the dominant role. The warming role is illustrated using the temperature change between perturbed and control simulation responses to CO2 or black carbon (BC) forcing via Community Earth System Model (CESM). It shows that an obvious warming in the TP is induced by the CO2 warming effect, and BC exhibits an amplifying effect on the warming. Therefore, the continuous warming in the TP was a result of uniform DIT warming over a large scale and enhanced RFT warming at a regional scale.
format article
author Jieru Ma
Xiaodan Guan
Ruixia Guo
Zewen Gan
Yongkun Xie
author_facet Jieru Ma
Xiaodan Guan
Ruixia Guo
Zewen Gan
Yongkun Xie
author_sort Jieru Ma
title Mechanism of non-appearance of hiatus in Tibetan Plateau
title_short Mechanism of non-appearance of hiatus in Tibetan Plateau
title_full Mechanism of non-appearance of hiatus in Tibetan Plateau
title_fullStr Mechanism of non-appearance of hiatus in Tibetan Plateau
title_full_unstemmed Mechanism of non-appearance of hiatus in Tibetan Plateau
title_sort mechanism of non-appearance of hiatus in tibetan plateau
publisher Nature Portfolio
publishDate 2017
url https://doaj.org/article/9cd0332315794204978dbcfbaafad541
work_keys_str_mv AT jieruma mechanismofnonappearanceofhiatusintibetanplateau
AT xiaodanguan mechanismofnonappearanceofhiatusintibetanplateau
AT ruixiaguo mechanismofnonappearanceofhiatusintibetanplateau
AT zewengan mechanismofnonappearanceofhiatusintibetanplateau
AT yongkunxie mechanismofnonappearanceofhiatusintibetanplateau
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