Trends of temperature and precipitation extremes in the Loess Plateau Region of China, 1961–2010
The spatial and temporal trends of 11 (7) temperature (precipitation) extreme indices are examined for the Loess Plateau Region (LPR) and its southeast and northwest sub-regions based on daily observations at 214 meteorological stations. Results show widespread significant warming trends for all the...
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description | The spatial and temporal trends of 11 (7) temperature (precipitation) extreme indices are examined for the Loess Plateau Region (LPR) and its southeast and northwest sub-regions based on daily observations at 214 meteorological stations. Results show widespread significant warming trends for all the temperature extremes except for the diurnal temperature range (DTR) and the lowest daily maximum temperature in each year (TXn) during 1961–2010. When regionally averaged, a significant warming trend is detected for all the indices except for DTR and TXn in the past 50 years. Compared with the entire LPR, a significant warming trend is detected for all the indices except for DTR and TXn over the southeast sub-region of LPR; while it is observed for all the indices over the northwest. The trends for these indices are generally stronger in the northwest than in the southeast in the past 50 years. In contrast, for precipitation indices, only a small percentage of areas show significant drying or wetting trends and, when regionally averaged, none of them displays significant trends during the past 50 years. On the sub-regional scale, however, a larger percentage of areas show significant drying trends for precipitation indices generally over the southeast relative to the entire LPR, and noticeably, the sub-regional average heavy precipitation (R10mm) and wet day precipitation (PRCPTOT) display significant decreasing trends during the past 50 years; whereas only a slightly larger percentage of areas show significant wetting trends for these indices over the northwest compared with the entire LPR, and when sub-regionally averaged, none of the indices have significant trends during the past 50 years. |
doi_str_mv | 10.1007/s00704-016-1820-z |
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Results show widespread significant warming trends for all the temperature extremes except for the diurnal temperature range (DTR) and the lowest daily maximum temperature in each year (TXn) during 1961–2010. When regionally averaged, a significant warming trend is detected for all the indices except for DTR and TXn in the past 50 years. Compared with the entire LPR, a significant warming trend is detected for all the indices except for DTR and TXn over the southeast sub-region of LPR; while it is observed for all the indices over the northwest. The trends for these indices are generally stronger in the northwest than in the southeast in the past 50 years. In contrast, for precipitation indices, only a small percentage of areas show significant drying or wetting trends and, when regionally averaged, none of them displays significant trends during the past 50 years. On the sub-regional scale, however, a larger percentage of areas show significant drying trends for precipitation indices generally over the southeast relative to the entire LPR, and noticeably, the sub-regional average heavy precipitation (R10mm) and wet day precipitation (PRCPTOT) display significant decreasing trends during the past 50 years; whereas only a slightly larger percentage of areas show significant wetting trends for these indices over the northwest compared with the entire LPR, and when sub-regionally averaged, none of the indices have significant trends during the past 50 years.</description><identifier>ISSN: 0177-798X</identifier><identifier>EISSN: 1434-4483</identifier><identifier>DOI: 10.1007/s00704-016-1820-z</identifier><language>eng</language><publisher>Vienna: Springer Vienna</publisher><subject>Aquatic Pollution ; Atmospheric precipitations ; Atmospheric Protection/Air Quality Control/Air Pollution ; Atmospheric Sciences ; Climate change ; Climate science ; Climatology ; Daily temperature range ; Daily temperatures ; Drying ; Earth and Environmental Science ; Earth Sciences ; Extreme values ; Extreme weather ; Heavy precipitation ; Loess ; Original Paper ; Plateaus ; Precipitation ; Precipitation (Meteorology) ; Temperature ; Temperature effects ; Temperature extremes ; Trends ; Waste Water Technology ; Water Management ; Water Pollution Control ; Weather stations ; Wetting</subject><ispartof>Theoretical and applied climatology, 2017-08, Vol.129 (3-4), p.949-963</ispartof><rights>Springer-Verlag Wien 2016</rights><rights>COPYRIGHT 2017 Springer</rights><rights>Theoretical and Applied Climatology is a copyright of Springer, 2017.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c389t-77a771b9db70e4845d9452f3ac66bb34f05b599ee2abf78759dec04a98fd612c3</citedby><cites>FETCH-LOGICAL-c389t-77a771b9db70e4845d9452f3ac66bb34f05b599ee2abf78759dec04a98fd612c3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00704-016-1820-z$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00704-016-1820-z$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Wang, Qi-xiang</creatorcontrib><creatorcontrib>Wang, Meng-ben</creatorcontrib><creatorcontrib>Fan, Xiao-hui</creatorcontrib><creatorcontrib>Zhang, Feng</creatorcontrib><creatorcontrib>Zhu, Shi-zhong</creatorcontrib><creatorcontrib>Zhao, Tian-liang</creatorcontrib><title>Trends of temperature and precipitation extremes in the Loess Plateau Region of China, 1961–2010</title><title>Theoretical and applied climatology</title><addtitle>Theor Appl Climatol</addtitle><description>The spatial and temporal trends of 11 (7) temperature (precipitation) extreme indices are examined for the Loess Plateau Region (LPR) and its southeast and northwest sub-regions based on daily observations at 214 meteorological stations. Results show widespread significant warming trends for all the temperature extremes except for the diurnal temperature range (DTR) and the lowest daily maximum temperature in each year (TXn) during 1961–2010. When regionally averaged, a significant warming trend is detected for all the indices except for DTR and TXn in the past 50 years. Compared with the entire LPR, a significant warming trend is detected for all the indices except for DTR and TXn over the southeast sub-region of LPR; while it is observed for all the indices over the northwest. The trends for these indices are generally stronger in the northwest than in the southeast in the past 50 years. In contrast, for precipitation indices, only a small percentage of areas show significant drying or wetting trends and, when regionally averaged, none of them displays significant trends during the past 50 years. On the sub-regional scale, however, a larger percentage of areas show significant drying trends for precipitation indices generally over the southeast relative to the entire LPR, and noticeably, the sub-regional average heavy precipitation (R10mm) and wet day precipitation (PRCPTOT) display significant decreasing trends during the past 50 years; whereas only a slightly larger percentage of areas show significant wetting trends for these indices over the northwest compared with the entire LPR, and when sub-regionally averaged, none of the indices have significant trends during the past 50 years.</description><subject>Aquatic Pollution</subject><subject>Atmospheric precipitations</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Atmospheric Sciences</subject><subject>Climate change</subject><subject>Climate science</subject><subject>Climatology</subject><subject>Daily temperature range</subject><subject>Daily temperatures</subject><subject>Drying</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Extreme values</subject><subject>Extreme weather</subject><subject>Heavy precipitation</subject><subject>Loess</subject><subject>Original Paper</subject><subject>Plateaus</subject><subject>Precipitation</subject><subject>Precipitation (Meteorology)</subject><subject>Temperature</subject><subject>Temperature effects</subject><subject>Temperature extremes</subject><subject>Trends</subject><subject>Waste Water Technology</subject><subject>Water Management</subject><subject>Water Pollution Control</subject><subject>Weather 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Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering collection</collection><collection>ProQuest Central Basic</collection><jtitle>Theoretical and applied climatology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Qi-xiang</au><au>Wang, Meng-ben</au><au>Fan, Xiao-hui</au><au>Zhang, Feng</au><au>Zhu, Shi-zhong</au><au>Zhao, Tian-liang</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Trends of temperature and precipitation extremes in the Loess Plateau Region of China, 1961–2010</atitle><jtitle>Theoretical and applied climatology</jtitle><stitle>Theor Appl Climatol</stitle><date>2017-08-01</date><risdate>2017</risdate><volume>129</volume><issue>3-4</issue><spage>949</spage><epage>963</epage><pages>949-963</pages><issn>0177-798X</issn><eissn>1434-4483</eissn><abstract>The spatial and temporal trends of 11 (7) temperature (precipitation) extreme indices are examined for the Loess Plateau Region (LPR) and its southeast and northwest sub-regions based on daily observations at 214 meteorological stations. Results show widespread significant warming trends for all the temperature extremes except for the diurnal temperature range (DTR) and the lowest daily maximum temperature in each year (TXn) during 1961–2010. When regionally averaged, a significant warming trend is detected for all the indices except for DTR and TXn in the past 50 years. Compared with the entire LPR, a significant warming trend is detected for all the indices except for DTR and TXn over the southeast sub-region of LPR; while it is observed for all the indices over the northwest. The trends for these indices are generally stronger in the northwest than in the southeast in the past 50 years. In contrast, for precipitation indices, only a small percentage of areas show significant drying or wetting trends and, when regionally averaged, none of them displays significant trends during the past 50 years. On the sub-regional scale, however, a larger percentage of areas show significant drying trends for precipitation indices generally over the southeast relative to the entire LPR, and noticeably, the sub-regional average heavy precipitation (R10mm) and wet day precipitation (PRCPTOT) display significant decreasing trends during the past 50 years; whereas only a slightly larger percentage of areas show significant wetting trends for these indices over the northwest compared with the entire LPR, and when sub-regionally averaged, none of the indices have significant trends during the past 50 years.</abstract><cop>Vienna</cop><pub>Springer Vienna</pub><doi>10.1007/s00704-016-1820-z</doi><tpages>15</tpages></addata></record> |
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subjects | Aquatic Pollution Atmospheric precipitations Atmospheric Protection/Air Quality Control/Air Pollution Atmospheric Sciences Climate change Climate science Climatology Daily temperature range Daily temperatures Drying Earth and Environmental Science Earth Sciences Extreme values Extreme weather Heavy precipitation Loess Original Paper Plateaus Precipitation Precipitation (Meteorology) Temperature Temperature effects Temperature extremes Trends Waste Water Technology Water Management Water Pollution Control Weather stations Wetting |
title | Trends of temperature and precipitation extremes in the Loess Plateau Region of China, 1961–2010 |
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