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A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia
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| Zeitschriftentitel: | Quarterly Journal of the Royal Meteorological Society |
|---|---|
| Personen und Körperschaften: | , , , , , , , |
| In: | Quarterly Journal of the Royal Meteorological Society, 144, 2018, 711, S. 604-613 |
| Format: | E-Article |
| Sprache: | Englisch |
| veröffentlicht: |
Wiley
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| Schlagwörter: |
| author_facet |
Zhao, Weihong Du, Haibo Wang, Lei He, Hong S. Wu, Zhengfang Liu, Kai Guo, Xiangyu Yang, Yue Zhao, Weihong Du, Haibo Wang, Lei He, Hong S. Wu, Zhengfang Liu, Kai Guo, Xiangyu Yang, Yue |
|---|---|
| author |
Zhao, Weihong Du, Haibo Wang, Lei He, Hong S. Wu, Zhengfang Liu, Kai Guo, Xiangyu Yang, Yue |
| spellingShingle |
Zhao, Weihong Du, Haibo Wang, Lei He, Hong S. Wu, Zhengfang Liu, Kai Guo, Xiangyu Yang, Yue Quarterly Journal of the Royal Meteorological Society A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia Atmospheric Science |
| author_sort |
zhao, weihong |
| spelling |
Zhao, Weihong Du, Haibo Wang, Lei He, Hong S. Wu, Zhengfang Liu, Kai Guo, Xiangyu Yang, Yue 0035-9009 1477-870X Wiley Atmospheric Science http://dx.doi.org/10.1002/qj.3234 <jats:p>Eurasia is one of the most sensitive areas to climate change in the world. Its western and eastern coasts are very likely to exhibit different temperature and precipitation variations in response to the global climate change. By using precipitation (<jats:styled-content style="fixed-case">PRCP</jats:styled-content>), maximum temperature (<jats:italic>T</jats:italic><jats:sub>max</jats:sub>), minimum temperature (<jats:italic>T</jats:italic><jats:sub>min</jats:sub>), and daily temperature range (<jats:styled-content style="fixed-case">DTR</jats:styled-content>) data from 333 meteorological stations in Western (<jats:styled-content style="fixed-case">WE</jats:styled-content>) and Eastern Eurasia (<jats:styled-content style="fixed-case">EE</jats:styled-content>), we quantitatively compared spatio‐temporal changes on both the seasonal and annual scales from 1961 to 2012. Results showed that <jats:styled-content style="fixed-case">PRCP</jats:styled-content> mainly exhibited increasing trends in northern <jats:styled-content style="fixed-case">WE</jats:styled-content> and decreasing trends in southern <jats:styled-content style="fixed-case">WE</jats:styled-content>, whereas <jats:styled-content style="fixed-case">PRCP</jats:styled-content> in <jats:styled-content style="fixed-case">EE</jats:styled-content> recorded an increase–decrease–increase trend from high to low latitudes. The increase of annual <jats:styled-content style="fixed-case">PRCP</jats:styled-content> in <jats:styled-content style="fixed-case">WE</jats:styled-content> was higher than that in <jats:styled-content style="fixed-case">EE</jats:styled-content>. On the seasonal scale, the <jats:styled-content style="fixed-case">PRCP</jats:styled-content> in <jats:styled-content style="fixed-case">WE</jats:styled-content> recorded an opposite trend from <jats:styled-content style="fixed-case">EE</jats:styled-content>. <jats:italic>T</jats:italic><jats:sub>max</jats:sub> and <jats:italic>T</jats:italic><jats:sub>min</jats:sub> significantly increased for almost all stations on the annual and seasonal scales, especially during the winter. Nevertheless, the increase of <jats:italic>T</jats:italic><jats:sub>min</jats:sub> was higher than that of <jats:italic>T</jats:italic><jats:sub>max</jats:sub> in <jats:styled-content style="fixed-case">EE</jats:styled-content>, resulting in a decreased <jats:styled-content style="fixed-case">DTR</jats:styled-content> on both the seasonal and annual scales. An reverse trend of <jats:styled-content style="fixed-case">DTR</jats:styled-content> was detected in <jats:styled-content style="fixed-case">WE</jats:styled-content>. Our results concluded that the Arctic Oscillation was the major large‐scale atmospheric circulation affecting the trends of <jats:styled-content style="fixed-case">PRCP</jats:styled-content> (negative correlation) and temperature (positive correlation) over <jats:styled-content style="fixed-case">WE</jats:styled-content> and <jats:styled-content style="fixed-case">EE</jats:styled-content>, and it might play an important role in future climate change.</jats:p> A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia Quarterly Journal of the Royal Meteorological Society |
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10.1002/qj.3234 |
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Online Free |
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| imprint |
Wiley, 2018 |
| imprint_str_mv |
Wiley, 2018 |
| issn |
0035-9009 1477-870X |
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0035-9009 1477-870X |
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2018 |
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Wiley |
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Quarterly Journal of the Royal Meteorological Society |
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| title |
A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia |
| title_unstemmed |
A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia |
| title_full |
A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia |
| title_fullStr |
A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia |
| title_full_unstemmed |
A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia |
| title_short |
A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia |
| title_sort |
a comparison of recent trends in precipitation and temperature over western and eastern eurasia |
| topic |
Atmospheric Science |
| url |
http://dx.doi.org/10.1002/qj.3234 |
| publishDate |
2018 |
| physical |
604-613 |
| description |
<jats:p>Eurasia is one of the most sensitive areas to climate change in the world. Its western and eastern coasts are very likely to exhibit different temperature and precipitation variations in response to the global climate change. By using precipitation (<jats:styled-content style="fixed-case">PRCP</jats:styled-content>), maximum temperature (<jats:italic>T</jats:italic><jats:sub>max</jats:sub>), minimum temperature (<jats:italic>T</jats:italic><jats:sub>min</jats:sub>), and daily temperature range (<jats:styled-content style="fixed-case">DTR</jats:styled-content>) data from 333 meteorological stations in Western (<jats:styled-content style="fixed-case">WE</jats:styled-content>) and Eastern Eurasia (<jats:styled-content style="fixed-case">EE</jats:styled-content>), we quantitatively compared spatio‐temporal changes on both the seasonal and annual scales from 1961 to 2012. Results showed that <jats:styled-content style="fixed-case">PRCP</jats:styled-content> mainly exhibited increasing trends in northern <jats:styled-content style="fixed-case">WE</jats:styled-content> and decreasing trends in southern <jats:styled-content style="fixed-case">WE</jats:styled-content>, whereas <jats:styled-content style="fixed-case">PRCP</jats:styled-content> in <jats:styled-content style="fixed-case">EE</jats:styled-content> recorded an increase–decrease–increase trend from high to low latitudes. The increase of annual <jats:styled-content style="fixed-case">PRCP</jats:styled-content> in <jats:styled-content style="fixed-case">WE</jats:styled-content> was higher than that in <jats:styled-content style="fixed-case">EE</jats:styled-content>. On the seasonal scale, the <jats:styled-content style="fixed-case">PRCP</jats:styled-content> in <jats:styled-content style="fixed-case">WE</jats:styled-content> recorded an opposite trend from <jats:styled-content style="fixed-case">EE</jats:styled-content>. <jats:italic>T</jats:italic><jats:sub>max</jats:sub> and <jats:italic>T</jats:italic><jats:sub>min</jats:sub> significantly increased for almost all stations on the annual and seasonal scales, especially during the winter. Nevertheless, the increase of <jats:italic>T</jats:italic><jats:sub>min</jats:sub> was higher than that of <jats:italic>T</jats:italic><jats:sub>max</jats:sub> in <jats:styled-content style="fixed-case">EE</jats:styled-content>, resulting in a decreased <jats:styled-content style="fixed-case">DTR</jats:styled-content> on both the seasonal and annual scales. An reverse trend of <jats:styled-content style="fixed-case">DTR</jats:styled-content> was detected in <jats:styled-content style="fixed-case">WE</jats:styled-content>. Our results concluded that the Arctic Oscillation was the major large‐scale atmospheric circulation affecting the trends of <jats:styled-content style="fixed-case">PRCP</jats:styled-content> (negative correlation) and temperature (positive correlation) over <jats:styled-content style="fixed-case">WE</jats:styled-content> and <jats:styled-content style="fixed-case">EE</jats:styled-content>, and it might play an important role in future climate change.</jats:p> |
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| author | Zhao, Weihong, Du, Haibo, Wang, Lei, He, Hong S., Wu, Zhengfang, Liu, Kai, Guo, Xiangyu, Yang, Yue |
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| description | <jats:p>Eurasia is one of the most sensitive areas to climate change in the world. Its western and eastern coasts are very likely to exhibit different temperature and precipitation variations in response to the global climate change. By using precipitation (<jats:styled-content style="fixed-case">PRCP</jats:styled-content>), maximum temperature (<jats:italic>T</jats:italic><jats:sub>max</jats:sub>), minimum temperature (<jats:italic>T</jats:italic><jats:sub>min</jats:sub>), and daily temperature range (<jats:styled-content style="fixed-case">DTR</jats:styled-content>) data from 333 meteorological stations in Western (<jats:styled-content style="fixed-case">WE</jats:styled-content>) and Eastern Eurasia (<jats:styled-content style="fixed-case">EE</jats:styled-content>), we quantitatively compared spatio‐temporal changes on both the seasonal and annual scales from 1961 to 2012. Results showed that <jats:styled-content style="fixed-case">PRCP</jats:styled-content> mainly exhibited increasing trends in northern <jats:styled-content style="fixed-case">WE</jats:styled-content> and decreasing trends in southern <jats:styled-content style="fixed-case">WE</jats:styled-content>, whereas <jats:styled-content style="fixed-case">PRCP</jats:styled-content> in <jats:styled-content style="fixed-case">EE</jats:styled-content> recorded an increase–decrease–increase trend from high to low latitudes. The increase of annual <jats:styled-content style="fixed-case">PRCP</jats:styled-content> in <jats:styled-content style="fixed-case">WE</jats:styled-content> was higher than that in <jats:styled-content style="fixed-case">EE</jats:styled-content>. On the seasonal scale, the <jats:styled-content style="fixed-case">PRCP</jats:styled-content> in <jats:styled-content style="fixed-case">WE</jats:styled-content> recorded an opposite trend from <jats:styled-content style="fixed-case">EE</jats:styled-content>. <jats:italic>T</jats:italic><jats:sub>max</jats:sub> and <jats:italic>T</jats:italic><jats:sub>min</jats:sub> significantly increased for almost all stations on the annual and seasonal scales, especially during the winter. Nevertheless, the increase of <jats:italic>T</jats:italic><jats:sub>min</jats:sub> was higher than that of <jats:italic>T</jats:italic><jats:sub>max</jats:sub> in <jats:styled-content style="fixed-case">EE</jats:styled-content>, resulting in a decreased <jats:styled-content style="fixed-case">DTR</jats:styled-content> on both the seasonal and annual scales. An reverse trend of <jats:styled-content style="fixed-case">DTR</jats:styled-content> was detected in <jats:styled-content style="fixed-case">WE</jats:styled-content>. Our results concluded that the Arctic Oscillation was the major large‐scale atmospheric circulation affecting the trends of <jats:styled-content style="fixed-case">PRCP</jats:styled-content> (negative correlation) and temperature (positive correlation) over <jats:styled-content style="fixed-case">WE</jats:styled-content> and <jats:styled-content style="fixed-case">EE</jats:styled-content>, and it might play an important role in future climate change.</jats:p> |
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| spelling | Zhao, Weihong Du, Haibo Wang, Lei He, Hong S. Wu, Zhengfang Liu, Kai Guo, Xiangyu Yang, Yue 0035-9009 1477-870X Wiley Atmospheric Science http://dx.doi.org/10.1002/qj.3234 <jats:p>Eurasia is one of the most sensitive areas to climate change in the world. Its western and eastern coasts are very likely to exhibit different temperature and precipitation variations in response to the global climate change. By using precipitation (<jats:styled-content style="fixed-case">PRCP</jats:styled-content>), maximum temperature (<jats:italic>T</jats:italic><jats:sub>max</jats:sub>), minimum temperature (<jats:italic>T</jats:italic><jats:sub>min</jats:sub>), and daily temperature range (<jats:styled-content style="fixed-case">DTR</jats:styled-content>) data from 333 meteorological stations in Western (<jats:styled-content style="fixed-case">WE</jats:styled-content>) and Eastern Eurasia (<jats:styled-content style="fixed-case">EE</jats:styled-content>), we quantitatively compared spatio‐temporal changes on both the seasonal and annual scales from 1961 to 2012. Results showed that <jats:styled-content style="fixed-case">PRCP</jats:styled-content> mainly exhibited increasing trends in northern <jats:styled-content style="fixed-case">WE</jats:styled-content> and decreasing trends in southern <jats:styled-content style="fixed-case">WE</jats:styled-content>, whereas <jats:styled-content style="fixed-case">PRCP</jats:styled-content> in <jats:styled-content style="fixed-case">EE</jats:styled-content> recorded an increase–decrease–increase trend from high to low latitudes. The increase of annual <jats:styled-content style="fixed-case">PRCP</jats:styled-content> in <jats:styled-content style="fixed-case">WE</jats:styled-content> was higher than that in <jats:styled-content style="fixed-case">EE</jats:styled-content>. On the seasonal scale, the <jats:styled-content style="fixed-case">PRCP</jats:styled-content> in <jats:styled-content style="fixed-case">WE</jats:styled-content> recorded an opposite trend from <jats:styled-content style="fixed-case">EE</jats:styled-content>. <jats:italic>T</jats:italic><jats:sub>max</jats:sub> and <jats:italic>T</jats:italic><jats:sub>min</jats:sub> significantly increased for almost all stations on the annual and seasonal scales, especially during the winter. Nevertheless, the increase of <jats:italic>T</jats:italic><jats:sub>min</jats:sub> was higher than that of <jats:italic>T</jats:italic><jats:sub>max</jats:sub> in <jats:styled-content style="fixed-case">EE</jats:styled-content>, resulting in a decreased <jats:styled-content style="fixed-case">DTR</jats:styled-content> on both the seasonal and annual scales. An reverse trend of <jats:styled-content style="fixed-case">DTR</jats:styled-content> was detected in <jats:styled-content style="fixed-case">WE</jats:styled-content>. Our results concluded that the Arctic Oscillation was the major large‐scale atmospheric circulation affecting the trends of <jats:styled-content style="fixed-case">PRCP</jats:styled-content> (negative correlation) and temperature (positive correlation) over <jats:styled-content style="fixed-case">WE</jats:styled-content> and <jats:styled-content style="fixed-case">EE</jats:styled-content>, and it might play an important role in future climate change.</jats:p> A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia Quarterly Journal of the Royal Meteorological Society |
| spellingShingle | Zhao, Weihong, Du, Haibo, Wang, Lei, He, Hong S., Wu, Zhengfang, Liu, Kai, Guo, Xiangyu, Yang, Yue, Quarterly Journal of the Royal Meteorological Society, A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia, Atmospheric Science |
| title | A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia |
| title_full | A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia |
| title_fullStr | A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia |
| title_full_unstemmed | A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia |
| title_short | A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia |
| title_sort | a comparison of recent trends in precipitation and temperature over western and eastern eurasia |
| title_unstemmed | A comparison of recent trends in precipitation and temperature over Western and Eastern Eurasia |
| topic | Atmospheric Science |
| url | http://dx.doi.org/10.1002/qj.3234 |