Patterns of Multiscale Temperature Variability over the Eastern and Central Tibetan Plateau During 1960-2008
Climate variability is an important inherent characteristic of climate and it varies on all timescales. Through examination of temperature variability on multiple temporal scales at 63 stations over the eastern and central Tibetan Plateau （TP） during 1960-2008, we find decreasing trends in daily and...
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| Published in | Acta meteorologica Sinica Vol. 27; no. 4; pp. 521 - 540 |
|---|---|
| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
Berlin/Heidelberg
Springer Berlin Heidelberg
01.08.2013
Institute of Geographic Sciences and Natural Resource Research, Chinese Academy of Sciences, Beijing 100101%China University of Petroleum,Qingdao,266580 |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0894-0525 2191-4788 |
| DOI | 10.1007/s13351-013-0407-1 |
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| Abstract | Climate variability is an important inherent characteristic of climate and it varies on all timescales. Through examination of temperature variability on multiple temporal scales at 63 stations over the eastern and central Tibetan Plateau （TP） during 1960-2008, we find decreasing trends in daily and intraannual temperature, especially in cold seasons （autumn and winter）. These changes are more sensitive than those in the eastern China coastal region at the same latitude and indicate an asymmetric change of temperature, with hourly, daily, and monthly trends in cold periods stronger than those in warm periods during the recent years. The variation of interannual temperature is complex, showing an increasing trend in autumn and winter and decreasing trend in spring and summer, which is similar to those in the northern polar region. The changes of multiscale variability of temperature are mainly related to changes of atmospheric water vapor, cloudiness, anthropogenic aerosols, monsoon-driven climate, and some local factors. To find the influences of local conditions on temperature variability, we analyze the effects of altitude, topography, and urbanization. The results show that elevation is strongly and positively related to diurnal temperature range （DTR） and slightly positively related to interannual temperature variability （IVT）, but intraannual temperature variability shows no clear elevation dependency. Topography and urbanization also play important roles in multiscale temperature variability. Finally, strong relationships are observed between temperature variability on each scale and different extreme indices. |
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| AbstractList | Climate variability is an important inherent characteristic of climate and it varies on all timescales. Through examination of temperature variability on multiple temporal scales at 63 stations over the eastern and central Tibetan Plateau （TP） during 1960-2008, we find decreasing trends in daily and intraannual temperature, especially in cold seasons （autumn and winter）. These changes are more sensitive than those in the eastern China coastal region at the same latitude and indicate an asymmetric change of temperature, with hourly, daily, and monthly trends in cold periods stronger than those in warm periods during the recent years. The variation of interannual temperature is complex, showing an increasing trend in autumn and winter and decreasing trend in spring and summer, which is similar to those in the northern polar region. The changes of multiscale variability of temperature are mainly related to changes of atmospheric water vapor, cloudiness, anthropogenic aerosols, monsoon-driven climate, and some local factors. To find the influences of local conditions on temperature variability, we analyze the effects of altitude, topography, and urbanization. The results show that elevation is strongly and positively related to diurnal temperature range （DTR） and slightly positively related to interannual temperature variability （IVT）, but intraannual temperature variability shows no clear elevation dependency. Topography and urbanization also play important roles in multiscale temperature variability. Finally, strong relationships are observed between temperature variability on each scale and different extreme indices. Climate variability is an important inherent characteristic of climate and it varies on all timescales. Through examination of temperature variability on multiple temporal scales at 63 stations over the eastern and central Tibetan Plateau (TP) during 1960–2008, we find decreasing trends in daily and intraannual temperature, especially in cold seasons (autumn and winter). These changes are more sensitive than those in the eastern China coastal region at the same latitude and indicate an asymmetric change of temperature, with hourly, daily, and monthly trends in cold periods stronger than those in warm periods during the recent years. The variation of interannual temperature is complex, showing an increasing trend in autumn and winter and decreasing trend in spring and summer, which is similar to those in the northern polar region. The changes of multiscale variability of temperature are mainly related to changes of atmospheric water vapor, cloudiness, anthropogenic aerosols, monsoon-driven climate, and some local factors. To find the influences of local conditions on temperature variability, we analyze the effects of altitude, topography, and urbanization. The results show that elevation is strongly and positively related to diurnal temperature range (DTR) and slightly positively related to interannual temperature variability (IVT), but intraannual temperature variability shows no clear elevation dependency. Topography and urbanization also play important roles in multiscale temperature variability. Finally, strong relationships are observed between temperature variability on each scale and different extreme indices. |
| Author | 宋辞 裴韬 周成虎 何亚文 |
| AuthorAffiliation | Institute of Geographic Sciences and Natural Resource Research, Chinese Academy of Sciences, Beijing 100101 China University of Petroleum, Qingdao 266580 |
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| CitedBy_id | crossref_primary_10_1002_joc_3935 crossref_primary_10_1002_joc_4722 |
| Cites_doi | 10.1126/science.277.5324.364 10.1007/s00376-010-9242-9 10.1016/0048-9697(95)04411-S 10.1016/j.gloplacha.2010.01.020 10.2151/jmsj.87.721 10.1007/s00382-008-0473-8 10.1017/CBO9780511803819 10.1175/3230.1 10.1029/2005JD006562 10.1175/JHM609.1 10.1038/nature02300 10.1007/s00382-004-0488-8 10.1175/1520-0442(2002)015<1555:RBCVAW>2.0.CO;2 10.1029/2006GL027946 10.1002/1097-0088(20001130)20:14<1729::AID-JOC556>3.0.CO;2-Y 10.1016/j.gloplacha.2009.03.017 10.1007/s10584-006-9218-z 10.1007/s11442-012-0936-z 10.1175/2007JCLI1384.1 10.1007/s00376-010-0018-z 10.1007/s00382-004-0409-x 10.1029/2005GL024108 10.1002/joc.590 10.1002/joc.1087 10.1007/BF03182914 10.1360/03wd0481 10.1175/1520-0442(2002)015<3586:TIOTNA>2.0.CO;2 10.3354/cr00985 10.1007/s12583-010-0017-0 10.1088/1748-9326/4/4/045202 10.1029/1999GL011016 10.1002/joc.3512 10.1029/2007GL032669 10.1088/1748-9326/5/1/015101 10.1029/2005GL023424 10.1007/s00376-009-9052-0 10.1002/joc.610 10.1002/hyp.6892 10.1007/s00376-010-0006-3 10.3354/cr01070 10.1007/s10584-006-9229-9 10.1038/377217a0 10.1007/s00382-005-0068-6 10.1007/s007040170032 10.1007/BF00139728 10.1002/joc.1006 10.1175/1520-0442(2002)015<2395:CICIIT>2.0.CO;2 10.1029/2007JD009389 10.1029/2005JD006915 10.1080/16742834.2009.11446802 |
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| Copyright | The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2013 Copyright © Wanfang Data Co. Ltd. All Rights Reserved. |
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| Keywords | multiscale temperature variability Tibetan Plateau topography effect altitude effect |
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| Notes | 11-2277/P SONG Ci, PEI Tao, ZHOU Chenghu, and HE Yawen（ 1 Institute of Geographic Sciences and Natural Resource Research, Chinese Academy of Sciences, Beijing 100101 2 China University of Petroleum, Qingdao 266580） multiscale temperature variability, Tibetan Plateau, altitude effect, topography effect Climate variability is an important inherent characteristic of climate and it varies on all timescales. Through examination of temperature variability on multiple temporal scales at 63 stations over the eastern and central Tibetan Plateau （TP） during 1960-2008, we find decreasing trends in daily and intraannual temperature, especially in cold seasons （autumn and winter）. These changes are more sensitive than those in the eastern China coastal region at the same latitude and indicate an asymmetric change of temperature, with hourly, daily, and monthly trends in cold periods stronger than those in warm periods during the recent years. The variation of interannual temperature is complex, showing an increasing trend in autumn and winter and decreasing trend in spring and summer, which is similar to those in the northern polar region. The changes of multiscale variability of temperature are mainly related to changes of atmospheric water vapor, cloudiness, anthropogenic aerosols, monsoon-driven climate, and some local factors. To find the influences of local conditions on temperature variability, we analyze the effects of altitude, topography, and urbanization. The results show that elevation is strongly and positively related to diurnal temperature range （DTR） and slightly positively related to interannual temperature variability （IVT）, but intraannual temperature variability shows no clear elevation dependency. Topography and urbanization also play important roles in multiscale temperature variability. Finally, strong relationships are observed between temperature variability on each scale and different extreme indices. |
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| Publisher | Springer Berlin Heidelberg Institute of Geographic Sciences and Natural Resource Research, Chinese Academy of Sciences, Beijing 100101%China University of Petroleum,Qingdao,266580 |
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| Title | Patterns of Multiscale Temperature Variability over the Eastern and Central Tibetan Plateau During 1960-2008 |
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