Validation and Application of Reanalysis Temperature Data over the Tibetan Plateau
The Tibetan Plateau has substantial impacts on the weather and climate of the Northern Hemisphere, due in large part to the thermal effects of the plateau surface. Surface temperature over the Tibetan Plateau is the most important parameter in determining these thermal effects. We present a method f...
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| Published in | Acta meteorologica Sinica Vol. 28; no. 1; pp. 139 - 149 |
|---|---|
| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
Heidelberg
The Chinese Meteorological Society
01.02.2014
LAPC & LA0R, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029 |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0894-0525 2191-4788 |
| DOI | 10.1007/s13351-014-3027-5 |
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| Abstract | The Tibetan Plateau has substantial impacts on the weather and climate of the Northern Hemisphere, due in large part to the thermal effects of the plateau surface. Surface temperature over the Tibetan Plateau is the most important parameter in determining these thermal effects. We present a method for verifying widely used reanalysis temperature products from NCEP-R2, ERA-Interim, and JRA-25 over the Tibetan Plateau, with the aim of obtaining a reliable picture of surface temperature and its changes over the plateau. Reanalysis data are validated against the topography elevation, satellite observations, and radiosonde data. ERA-Interim provides the most reliable estimates of Tibetan Plateau surface temperature among these three reanalyses. We therefore use this dataset to study the climatology and trends of surface temperature over the Tibetan Plateau. ERA-Interim data indicate a dramatic warming over the Tibetan Plateau from 1979 to 2010, with warming rates of 0.33℃ per decade in annual mean temperature, 0.22℃ per decade in summer and 0.4℃ per decade in winter mean temperatures. Comparison with the results of previous studies suggests that surface warming over the Tibetan Plateau has accelerated during the past 30 years. This warming is distributed heterogeneously across the Tibetan Plateau, possibly due to topographic effects. |
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| AbstractList | The Tibetan Plateau has substantial impacts on the weather and climate of the Northern Hemisphere, due in large part to the thermal effects of the plateau surface. Surface temperature over the Tibetan Plateau is the most important parameter in determining these thermal effects. We present a method for verifying widely used reanalysis temperature products from NCEP-R2, ERA-Interim, and JRA-25 over the Tibetan Plateau, with the aim of obtaining a reliable picture of surface temperature and its changes over the plateau. Reanalysis data are validated against the topography elevation, satellite observations, and radiosonde data. ERA-Interim provides the most reliable estimates of Tibetan Plateau surface temperature among these three reanalyses. We therefore use this dataset to study the climatology and trends of surface temperature over the Tibetan Plateau. ERA-Interim data indicate a dramatic warming over the Tibetan Plateau from 1979 to 2010, with warming rates of 0.33 degree C per decade in annual mean temperature, 0.22 degree C per decade in summer and 0.47 degree C per decade in winter mean temperatures. Comparison with the results of previous studies suggests that surface warming over the Tibetan Plateau has accelerated during the past 30 years. This warming is distributed heterogeneously across the Tibetan Plateau, possibly due to topographic effects. The Tibetan Plateau has substantial impacts on the weather and climate of the Northern Hemisphere, due in large part to the thermal eff ects of the plateau surface. Surface temperature over the Tibetan Plateau is the most important parameter in determining these thermal eff ects. We present a method for verifying widely used reanalysis temperature products from NCEP-R2, ERA-Interim, and JRA-25 over the Tibetan Plateau, with the aim of obtaining a reliable picture of surface temperature and its changes over the plateau. Reanalysis data are validated against the topography elevation, satellite observations, and radiosonde data. ERA-Interim provides the most reliable estimates of Tibetan Plateau surface temperature among these three reanalyses. We therefore use this dataset to study the climatology and trends of surface temperature over the Tibetan Plateau. ERA-Interim data indicate a dramatic warming over the Tibetan Plateau from 1979 to 2010, with warming rates of 0.33℃per decade in annual mean temperature, 0.22℃per decade in summer and 0.47℃ per decade in winter mean temperatures. Comparison with the results of previous studies suggests that surface warming over the Tibetan Plateau has accelerated during the past 30 years. This warming is distributed heterogeneously across the Tibetan Plateau, possibly due to topographic eff ects. The Tibetan Plateau has substantial impacts on the weather and climate of the Northern Hemisphere, due in large part to the thermal effects of the plateau surface. Surface temperature over the Tibetan Plateau is the most important parameter in determining these thermal effects. We present a method for verifying widely used reanalysis temperature products from NCEP-R2, ERA-Interim, and JRA-25 over the Tibetan Plateau, with the aim of obtaining a reliable picture of surface temperature and its changes over the plateau. Reanalysis data are validated against the topography elevation, satellite observations, and radiosonde data. ERA-Interim provides the most reliable estimates of Tibetan Plateau surface temperature among these three reanalyses. We therefore use this dataset to study the climatology and trends of surface temperature over the Tibetan Plateau. ERA-Interim data indicate a dramatic warming over the Tibetan Plateau from 1979 to 2010, with warming rates of 0.33°C per decade in annual mean temperature, 0.22°C per decade in summer and 0.47°C per decade in winter mean temperatures. Comparison with the results of previous studies suggests that surface warming over the Tibetan Plateau has accelerated during the past 30 years. This warming is distributed heterogeneously across the Tibetan Plateau, possibly due to topographic effects. The Tibetan Plateau has substantial impacts on the weather and climate of the Northern Hemisphere, due in large part to the thermal effects of the plateau surface. Surface temperature over the Tibetan Plateau is the most important parameter in determining these thermal effects. We present a method for verifying widely used reanalysis temperature products from NCEP-R2, ERA-Interim, and JRA-25 over the Tibetan Plateau, with the aim of obtaining a reliable picture of surface temperature and its changes over the plateau. Reanalysis data are validated against the topography elevation, satellite observations, and radiosonde data. ERA-Interim provides the most reliable estimates of Tibetan Plateau surface temperature among these three reanalyses. We therefore use this dataset to study the climatology and trends of surface temperature over the Tibetan Plateau. ERA-Interim data indicate a dramatic warming over the Tibetan Plateau from 1979 to 2010, with warming rates of 0.33℃ per decade in annual mean temperature, 0.22℃ per decade in summer and 0.4℃ per decade in winter mean temperatures. Comparison with the results of previous studies suggests that surface warming over the Tibetan Plateau has accelerated during the past 30 years. This warming is distributed heterogeneously across the Tibetan Plateau, possibly due to topographic effects. |
| Author | 邹捍 朱金焕 周立波 李鹏 马舒坡 |
| AuthorAffiliation | LAPC ＆LAOR, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029 |
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| CitedBy_id | crossref_primary_10_1002_joc_8176 crossref_primary_10_1007_s00704_021_03798_4 crossref_primary_10_1109_JSTARS_2017_2787191 crossref_primary_10_1007_s00382_024_07418_5 crossref_primary_10_1007_s11629_022_7361_2 crossref_primary_10_5194_tc_13_2221_2019 crossref_primary_10_1002_2016JD026237 crossref_primary_10_1002_2015JD024523 crossref_primary_10_1080_20964471_2023_2277551 crossref_primary_10_1002_hyp_11346 crossref_primary_10_1007_s00382_022_06518_4 crossref_primary_10_1080_07055900_2020_1800444 crossref_primary_10_1109_JSTARS_2023_3347202 crossref_primary_10_1155_2019_3160327 crossref_primary_10_1007_s12040_020_01409_w |
| Cites_doi | 10.1002/1097-0088(20001130)20:14<1729::AID-JOC556>3.0.CO;2-Y 10.1007/s40333-013-0138-2 10.1029/96GL00767 10.2151/jmsj.85.369 10.1029/2008GL034330 10.1029/2006GL027946 10.1256/qj.04.176 10.1016/j.rse.2006.06.026 10.1175/BAMS-83-11-1631 10.1073/pnas.0400357101 10.1016/j.rse.2012.10.034 10.1175/2009MWR2950.1 10.1038/nature01675 10.1029/2007JD009549 10.1175/2008JAMC1741.1 10.1002/joc.3512 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2 10.1002/qj.828 10.1007/s00376-007-0954-4 10.1007/s11430-009-0194-9 10.1088/1748-9326/6/4/045206 10.1007/s11434-009-0613-5 10.1088/1748-9326/5/1/015101 10.1029/2004JD005230 10.2151/jmsj1965.70.1B_319 |
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| Copyright | The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2014 Copyright © Wanfang Data Co. Ltd. All Rights Reserved. |
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| Notes | The Tibetan Plateau has substantial impacts on the weather and climate of the Northern Hemisphere, due in large part to the thermal effects of the plateau surface. Surface temperature over the Tibetan Plateau is the most important parameter in determining these thermal effects. We present a method for verifying widely used reanalysis temperature products from NCEP-R2, ERA-Interim, and JRA-25 over the Tibetan Plateau, with the aim of obtaining a reliable picture of surface temperature and its changes over the plateau. Reanalysis data are validated against the topography elevation, satellite observations, and radiosonde data. ERA-Interim provides the most reliable estimates of Tibetan Plateau surface temperature among these three reanalyses. We therefore use this dataset to study the climatology and trends of surface temperature over the Tibetan Plateau. ERA-Interim data indicate a dramatic warming over the Tibetan Plateau from 1979 to 2010, with warming rates of 0.33℃ per decade in annual mean temperature, 0.22℃ per decade in summer and 0.4℃ per decade in winter mean temperatures. Comparison with the results of previous studies suggests that surface warming over the Tibetan Plateau has accelerated during the past 30 years. This warming is distributed heterogeneously across the Tibetan Plateau, possibly due to topographic effects. 11-2277/P Tibetan Plateau, reanalysis, surface temperature, temperature trend ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 ObjectType-Article-2 ObjectType-Feature-1 |
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| Title | Validation and Application of Reanalysis Temperature Data over the Tibetan Plateau |
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