Quantitative characterization of climate change and its impact on aeolian desertification: a case study in northwest Shanxi of China
Aeolian desertification, a serious degradation of soil and vegetation, is one of the most important issues in arid and semi-arid regions in terms of society/economy and environment. However, there still remains problematic on the study of climate change and its impact on aeolian desertification in t...
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| Veröffentlicht in: | Environmental earth sciences 2021-04, Vol.80 (7), Article 242 |
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| description | Aeolian desertification, a serious degradation of soil and vegetation, is one of the most important issues in arid and semi-arid regions in terms of society/economy and environment. However, there still remains problematic on the study of climate change and its impact on aeolian desertification in the such region. To reverse aeolian desertified land (ADL), it is necessary to identify the causes of ADL. The paper uses meteorological data to characterize climate change and its impact on ADL during 1970–2015 with the method of geostatistics, and the results showed that the climate tended to be warmer and drier. The linear trend rates of annual mean temperature for the whole year (WY), winter half year (WHY), and summer half year (SHY) were 0.24 °C (10 a)
−1
, 0.25 °C (10 a)
−1
, and 0.18 °C (10 a)
−1
, respectively. The linear trend rates of average precipitation were − 8.29 mm (10 a)
−1
, 2.69 mm (10 a)
−1
, and − 8.27 mm (10 a)
−1
, respectively. Rising temperatures in WY, WHY, and SHY lead to increase topsoil evaporation and may trigger ADL development. However, the decreasing precipitation in SHY weakened soil erosion, and the increasing precipitation with a rate of 0.26 mm a
−1
in WHY improved the soil moisture content. Therefore, our results show that climatic change has a relatively high sensitivity, especially in WHY, to the expansion or reversal of ADL in semi-arid regions. |
| doi_str_mv | 10.1007/s12665-021-09557-y |
| format | Article |
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−1
, 0.25 °C (10 a)
−1
, and 0.18 °C (10 a)
−1
, respectively. The linear trend rates of average precipitation were − 8.29 mm (10 a)
−1
, 2.69 mm (10 a)
−1
, and − 8.27 mm (10 a)
−1
, respectively. Rising temperatures in WY, WHY, and SHY lead to increase topsoil evaporation and may trigger ADL development. However, the decreasing precipitation in SHY weakened soil erosion, and the increasing precipitation with a rate of 0.26 mm a
−1
in WHY improved the soil moisture content. Therefore, our results show that climatic change has a relatively high sensitivity, especially in WHY, to the expansion or reversal of ADL in semi-arid regions.</description><identifier>ISSN: 1866-6280</identifier><identifier>EISSN: 1866-6299</identifier><identifier>DOI: 10.1007/s12665-021-09557-y</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Arid regions ; Arid zones ; Biogeosciences ; Climate change ; Climate studies ; Desertification ; Earth and Environmental Science ; Earth Sciences ; Environmental Science and Engineering ; Evaporation ; Geochemistry ; Geology ; Geostatistics ; Hydrology/Water Resources ; Mean temperatures ; Meteorological data ; Moisture content ; Original Article ; Precipitation ; Semi arid areas ; Semiarid lands ; Semiarid zones ; Soil degradation ; Soil erosion ; Soil improvement ; Soil moisture ; Soil moisture content ; Temperature rise ; Terrestrial Pollution ; Topsoil ; Water content</subject><ispartof>Environmental earth sciences, 2021-04, Vol.80 (7), Article 242</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2021</rights><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2021.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a342t-eddfe64eada3533a18e9d9ff3b12666a8255d5b4833d6c5d2085a2ed2d529023</citedby><cites>FETCH-LOGICAL-a342t-eddfe64eada3533a18e9d9ff3b12666a8255d5b4833d6c5d2085a2ed2d529023</cites><orcidid>0000-0002-6730-5429</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12665-021-09557-y$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12665-021-09557-y$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Xue, Zhanjin</creatorcontrib><creatorcontrib>Qin, Zuodong</creatorcontrib><creatorcontrib>Cheng, Fangqin</creatorcontrib><creatorcontrib>Ding, Guangwei</creatorcontrib><creatorcontrib>Yan, Junxia</creatorcontrib><title>Quantitative characterization of climate change and its impact on aeolian desertification: a case study in northwest Shanxi of China</title><title>Environmental earth sciences</title><addtitle>Environ Earth Sci</addtitle><description>Aeolian desertification, a serious degradation of soil and vegetation, is one of the most important issues in arid and semi-arid regions in terms of society/economy and environment. However, there still remains problematic on the study of climate change and its impact on aeolian desertification in the such region. To reverse aeolian desertified land (ADL), it is necessary to identify the causes of ADL. The paper uses meteorological data to characterize climate change and its impact on ADL during 1970–2015 with the method of geostatistics, and the results showed that the climate tended to be warmer and drier. The linear trend rates of annual mean temperature for the whole year (WY), winter half year (WHY), and summer half year (SHY) were 0.24 °C (10 a)
−1
, 0.25 °C (10 a)
−1
, and 0.18 °C (10 a)
−1
, respectively. The linear trend rates of average precipitation were − 8.29 mm (10 a)
−1
, 2.69 mm (10 a)
−1
, and − 8.27 mm (10 a)
−1
, respectively. Rising temperatures in WY, WHY, and SHY lead to increase topsoil evaporation and may trigger ADL development. However, the decreasing precipitation in SHY weakened soil erosion, and the increasing precipitation with a rate of 0.26 mm a
−1
in WHY improved the soil moisture content. Therefore, our results show that climatic change has a relatively high sensitivity, especially in WHY, to the expansion or reversal of ADL in semi-arid regions.</description><subject>Arid regions</subject><subject>Arid zones</subject><subject>Biogeosciences</subject><subject>Climate change</subject><subject>Climate studies</subject><subject>Desertification</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Environmental Science and Engineering</subject><subject>Evaporation</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Geostatistics</subject><subject>Hydrology/Water Resources</subject><subject>Mean temperatures</subject><subject>Meteorological data</subject><subject>Moisture content</subject><subject>Original Article</subject><subject>Precipitation</subject><subject>Semi arid areas</subject><subject>Semiarid lands</subject><subject>Semiarid zones</subject><subject>Soil degradation</subject><subject>Soil erosion</subject><subject>Soil improvement</subject><subject>Soil moisture</subject><subject>Soil moisture content</subject><subject>Temperature rise</subject><subject>Terrestrial Pollution</subject><subject>Topsoil</subject><subject>Water content</subject><issn>1866-6280</issn><issn>1866-6299</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kEtPAyEYRYnRxEb7B1yRuB7lMdDBnWl8JU2MsXvydWAsTctUYNRx7Q-XdozuZAOBc-9HDkJnlFxQQiaXkTIpRUEYLYgSYlL0B2hEKykLyZQ6_D1X5BiNY1yRvDjlisgR-nrqwCeXILk3i-slBKiTDe4zX7Qetw2u124Daf_mXywGb7BLEbvNNpM4M2DbtQOPjY02JNe4ep-9woBriBbH1JkeO499G9Ly3caEn3PXh9u1T5fOwyk6amAd7fhnP0Hz25v59L6YPd49TK9nBfCSpcIa01hZWjDABedAK6uMahq-2AmQUDEhjFiUFedG1sIwUglg1jAjmCKMn6DzoXYb2tcu_0Ov2i74PFEzQagUJWeTTLGBqkMbY7CN3oZsIPSaEr3zrQffOvvWe9-6zyE-hGKGs6bwV_1P6htgPIXz</recordid><startdate>20210401</startdate><enddate>20210401</enddate><creator>Xue, Zhanjin</creator><creator>Qin, Zuodong</creator><creator>Cheng, Fangqin</creator><creator>Ding, Guangwei</creator><creator>Yan, Junxia</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-6730-5429</orcidid></search><sort><creationdate>20210401</creationdate><title>Quantitative characterization of climate change and its impact on aeolian desertification: a case study in northwest Shanxi of China</title><author>Xue, Zhanjin ; Qin, Zuodong ; Cheng, Fangqin ; Ding, Guangwei ; Yan, Junxia</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a342t-eddfe64eada3533a18e9d9ff3b12666a8255d5b4833d6c5d2085a2ed2d529023</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Arid regions</topic><topic>Arid zones</topic><topic>Biogeosciences</topic><topic>Climate change</topic><topic>Climate studies</topic><topic>Desertification</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Environmental Science and Engineering</topic><topic>Evaporation</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Geostatistics</topic><topic>Hydrology/Water Resources</topic><topic>Mean temperatures</topic><topic>Meteorological data</topic><topic>Moisture content</topic><topic>Original Article</topic><topic>Precipitation</topic><topic>Semi arid areas</topic><topic>Semiarid lands</topic><topic>Semiarid zones</topic><topic>Soil degradation</topic><topic>Soil erosion</topic><topic>Soil improvement</topic><topic>Soil moisture</topic><topic>Soil moisture content</topic><topic>Temperature rise</topic><topic>Terrestrial Pollution</topic><topic>Topsoil</topic><topic>Water content</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Xue, Zhanjin</creatorcontrib><creatorcontrib>Qin, Zuodong</creatorcontrib><creatorcontrib>Cheng, Fangqin</creatorcontrib><creatorcontrib>Ding, Guangwei</creatorcontrib><creatorcontrib>Yan, Junxia</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Environmental earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Xue, Zhanjin</au><au>Qin, Zuodong</au><au>Cheng, Fangqin</au><au>Ding, Guangwei</au><au>Yan, Junxia</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Quantitative characterization of climate change and its impact on aeolian desertification: a case study in northwest Shanxi of China</atitle><jtitle>Environmental earth sciences</jtitle><stitle>Environ Earth Sci</stitle><date>2021-04-01</date><risdate>2021</risdate><volume>80</volume><issue>7</issue><artnum>242</artnum><issn>1866-6280</issn><eissn>1866-6299</eissn><abstract>Aeolian desertification, a serious degradation of soil and vegetation, is one of the most important issues in arid and semi-arid regions in terms of society/economy and environment. However, there still remains problematic on the study of climate change and its impact on aeolian desertification in the such region. To reverse aeolian desertified land (ADL), it is necessary to identify the causes of ADL. The paper uses meteorological data to characterize climate change and its impact on ADL during 1970–2015 with the method of geostatistics, and the results showed that the climate tended to be warmer and drier. The linear trend rates of annual mean temperature for the whole year (WY), winter half year (WHY), and summer half year (SHY) were 0.24 °C (10 a)
−1
, 0.25 °C (10 a)
−1
, and 0.18 °C (10 a)
−1
, respectively. The linear trend rates of average precipitation were − 8.29 mm (10 a)
−1
, 2.69 mm (10 a)
−1
, and − 8.27 mm (10 a)
−1
, respectively. Rising temperatures in WY, WHY, and SHY lead to increase topsoil evaporation and may trigger ADL development. However, the decreasing precipitation in SHY weakened soil erosion, and the increasing precipitation with a rate of 0.26 mm a
−1
in WHY improved the soil moisture content. Therefore, our results show that climatic change has a relatively high sensitivity, especially in WHY, to the expansion or reversal of ADL in semi-arid regions.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s12665-021-09557-y</doi><orcidid>https://orcid.org/0000-0002-6730-5429</orcidid></addata></record> |
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| subjects | Arid regions Arid zones Biogeosciences Climate change Climate studies Desertification Earth and Environmental Science Earth Sciences Environmental Science and Engineering Evaporation Geochemistry Geology Geostatistics Hydrology/Water Resources Mean temperatures Meteorological data Moisture content Original Article Precipitation Semi arid areas Semiarid lands Semiarid zones Soil degradation Soil erosion Soil improvement Soil moisture Soil moisture content Temperature rise Terrestrial Pollution Topsoil Water content |
| title | Quantitative characterization of climate change and its impact on aeolian desertification: a case study in northwest Shanxi of China |
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