Significantly lower summer minimum temperature warming trend on the southern Tibetan Plateau than over the Eurasian continent since the Industrial Revolution
Summer temperature dominates environmental degradation and water resource availability on the Tibetan Plateau (TP), affecting glacier melting, permafrost degradation, desertification and streamflow, etc. Extending summer temperature records back before the instrumental period is fundamentally import...
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ftdoajarticles:oai:doaj.org/article:9fb11f5e73684fba9b998bee795bf8df 2023-09-05T13:22:34+02:00 Significantly lower summer minimum temperature warming trend on the southern Tibetan Plateau than over the Eurasian continent since the Industrial Revolution Chunming Shi Kaicun Wang Cheng Sun Yuandong Zhang Yanyi He Xiaoxu Wu Cong Gao Guocan Wu Lifu Shu 2019-01-01T00:00:00Z https://doi.org/10.1088/1748-9326/ab55fc https://doaj.org/article/9fb11f5e73684fba9b998bee795bf8df EN eng IOP Publishing https://doi.org/10.1088/1748-9326/ab55fc https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/ab55fc 1748-9326 https://doaj.org/article/9fb11f5e73684fba9b998bee795bf8df Environmental Research Letters, Vol 14, Iss 12, p 124033 (2019) Tibetan Plateau warming trend palaeoclimate minimum temperature CMIP5 tree ring Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 article 2019 ftdoajarticles https://doi.org/10.1088/1748-9326/ab55fc 2023-08-13T00:37:11Z Summer temperature dominates environmental degradation and water resource availability on the Tibetan Plateau (TP), affecting glacier melting, permafrost degradation, desertification and streamflow, etc. Extending summer temperature records back before the instrumental period is fundamentally important for climatic and environmental studies over long timescales. By pooling 39 tree-ring width records from the TP that show significant ( P < 0.05) correlations with the summer (June–August) minimum temperature (MinT) of the nearest grid point, we reconstructed a 366-year summer MinT record for the southern TP (STP). Reconstructed and instrumental data are highly coherent within the 1950–2010 calibration interval ( R ^2 = 0.50, P < 0.001). The reconstruction captures major temperature anomalies, such as the coldest interval of the 1810s–1820s and unprecedented warming since the 1990s. We found that the linear trends of the instrumental and reconstructed STP summer MinTs are significantly lower than those for the larger Eurasian continent over the periods 1950–2010 and 1850–1950, respectively. The lower warming rate of STP summer MinT since 1850 could be due to increased evaporative cooling, and the absence of warming enhancement factors such as snow-albedo and energy-absorbing aerosols in summer. The reconstructed summer warming rate for the STP appears to be significantly overestimated by the ensemble mean of the Coupled Model Intercomparison Project Phase 5 (CMIP5) historical simulation. Article in Journal/Newspaper permafrost Directory of Open Access Journals: DOAJ Articles Environmental Research Letters 14 12 124033 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Tibetan Plateau warming trend palaeoclimate minimum temperature CMIP5 tree ring Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
spellingShingle |
Tibetan Plateau warming trend palaeoclimate minimum temperature CMIP5 tree ring Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 Chunming Shi Kaicun Wang Cheng Sun Yuandong Zhang Yanyi He Xiaoxu Wu Cong Gao Guocan Wu Lifu Shu Significantly lower summer minimum temperature warming trend on the southern Tibetan Plateau than over the Eurasian continent since the Industrial Revolution |
topic_facet |
Tibetan Plateau warming trend palaeoclimate minimum temperature CMIP5 tree ring Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
description |
Summer temperature dominates environmental degradation and water resource availability on the Tibetan Plateau (TP), affecting glacier melting, permafrost degradation, desertification and streamflow, etc. Extending summer temperature records back before the instrumental period is fundamentally important for climatic and environmental studies over long timescales. By pooling 39 tree-ring width records from the TP that show significant ( P < 0.05) correlations with the summer (June–August) minimum temperature (MinT) of the nearest grid point, we reconstructed a 366-year summer MinT record for the southern TP (STP). Reconstructed and instrumental data are highly coherent within the 1950–2010 calibration interval ( R ^2 = 0.50, P < 0.001). The reconstruction captures major temperature anomalies, such as the coldest interval of the 1810s–1820s and unprecedented warming since the 1990s. We found that the linear trends of the instrumental and reconstructed STP summer MinTs are significantly lower than those for the larger Eurasian continent over the periods 1950–2010 and 1850–1950, respectively. The lower warming rate of STP summer MinT since 1850 could be due to increased evaporative cooling, and the absence of warming enhancement factors such as snow-albedo and energy-absorbing aerosols in summer. The reconstructed summer warming rate for the STP appears to be significantly overestimated by the ensemble mean of the Coupled Model Intercomparison Project Phase 5 (CMIP5) historical simulation. |
format |
Article in Journal/Newspaper |
author |
Chunming Shi Kaicun Wang Cheng Sun Yuandong Zhang Yanyi He Xiaoxu Wu Cong Gao Guocan Wu Lifu Shu |
author_facet |
Chunming Shi Kaicun Wang Cheng Sun Yuandong Zhang Yanyi He Xiaoxu Wu Cong Gao Guocan Wu Lifu Shu |
author_sort |
Chunming Shi |
title |
Significantly lower summer minimum temperature warming trend on the southern Tibetan Plateau than over the Eurasian continent since the Industrial Revolution |
title_short |
Significantly lower summer minimum temperature warming trend on the southern Tibetan Plateau than over the Eurasian continent since the Industrial Revolution |
title_full |
Significantly lower summer minimum temperature warming trend on the southern Tibetan Plateau than over the Eurasian continent since the Industrial Revolution |
title_fullStr |
Significantly lower summer minimum temperature warming trend on the southern Tibetan Plateau than over the Eurasian continent since the Industrial Revolution |
title_full_unstemmed |
Significantly lower summer minimum temperature warming trend on the southern Tibetan Plateau than over the Eurasian continent since the Industrial Revolution |
title_sort |
significantly lower summer minimum temperature warming trend on the southern tibetan plateau than over the eurasian continent since the industrial revolution |
publisher |
IOP Publishing |
publishDate |
2019 |
url |
https://doi.org/10.1088/1748-9326/ab55fc https://doaj.org/article/9fb11f5e73684fba9b998bee795bf8df |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Environmental Research Letters, Vol 14, Iss 12, p 124033 (2019) |
op_relation |
https://doi.org/10.1088/1748-9326/ab55fc https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/ab55fc 1748-9326 https://doaj.org/article/9fb11f5e73684fba9b998bee795bf8df |
op_doi |
https://doi.org/10.1088/1748-9326/ab55fc |
container_title |
Environmental Research Letters |
container_volume |
14 |
container_issue |
12 |
container_start_page |
124033 |
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1776203074585493504 |