Evaluating the effects of heatwave events on hydrological processes in the contiguous United States (2003–2022)
•Rainfall leads to increased humidity and a subsequent end to the heatwave.•Post- heatwave periods witness a notable decrease in water storage.•Heatwave conclusions correspond with heightened rainfall and increased runoff.•Rainfall is more probable post- heatwave than in non– heatwave intervals. Ext...
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Veröffentlicht in: | Journal of hydrology (Amsterdam) 2024-06, Vol.637, p.131368, Article 131368 |
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creator | Hao, Yuefeng Mao, Jiafu Jin, Mingzhou Wang, Yaoping Tang, Rongyun Lee, Zhe Weng |
description | •Rainfall leads to increased humidity and a subsequent end to the heatwave.•Post- heatwave periods witness a notable decrease in water storage.•Heatwave conclusions correspond with heightened rainfall and increased runoff.•Rainfall is more probable post- heatwave than in non– heatwave intervals.
Extreme heat and drought conditions are affecting water availability in many regions worldwide, leading to negative impacts on human societies, agriculture, and ecosystems. However, current research lacks comprehensive spatiotemporal analysis examining the interplay between multiple hydrological factors and heatwave events, especially in the context of climate change. This research broadly pertains to understanding the dynamics of hydrological factors and their potential responses to heatwave during warm seasons across the contiguous United States for the period from 2003 to 2022. Utilizing data from the Global Land Data Assimilation System (GLDAS), we analyzed surface runoff, evapotranspiration (ET), precipitation, Groundwater Storage (GWS), Root Zone Soil Moisture (RZSM), and Total Water Storage (TWS) to discern annual patterns and the impacts of heatwave. The spatial patterns of heatwave highlighted a higher occurrence in the western, central, and northeastern U.S., with longer average durations in the western and south-central regions. These events are predominantly dry, characterized by low Relative Humidity (RH), except in the southeastern U.S., where heatwave coincide with high RH levels. Post-heatwave analysis indicated a reduction in GWS, TWS, RZSM, and ET, alongside an increase in surface runoff, RH, and precipitation. An in-depth examination of rainfall and temperature dynamics during heatwave revealed weak correlations between rainfall and temperature, as well as between rainfall and heatwave duration, highlighting the complex nature of these interactions. The study also found an enhanced probability of rainfall following heatwave, particularly in the eastern regions, drawing attention to the potential for increased flood risks post-heatwave. Our findings contribute to the growing body of knowledge on the impacts of heatwave on hydrological factors, providing valuable insights for climate change adaptation and water resource management strategies. |
doi_str_mv | 10.1016/j.jhydrol.2024.131368 |
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Extreme heat and drought conditions are affecting water availability in many regions worldwide, leading to negative impacts on human societies, agriculture, and ecosystems. However, current research lacks comprehensive spatiotemporal analysis examining the interplay between multiple hydrological factors and heatwave events, especially in the context of climate change. This research broadly pertains to understanding the dynamics of hydrological factors and their potential responses to heatwave during warm seasons across the contiguous United States for the period from 2003 to 2022. Utilizing data from the Global Land Data Assimilation System (GLDAS), we analyzed surface runoff, evapotranspiration (ET), precipitation, Groundwater Storage (GWS), Root Zone Soil Moisture (RZSM), and Total Water Storage (TWS) to discern annual patterns and the impacts of heatwave. The spatial patterns of heatwave highlighted a higher occurrence in the western, central, and northeastern U.S., with longer average durations in the western and south-central regions. These events are predominantly dry, characterized by low Relative Humidity (RH), except in the southeastern U.S., where heatwave coincide with high RH levels. Post-heatwave analysis indicated a reduction in GWS, TWS, RZSM, and ET, alongside an increase in surface runoff, RH, and precipitation. An in-depth examination of rainfall and temperature dynamics during heatwave revealed weak correlations between rainfall and temperature, as well as between rainfall and heatwave duration, highlighting the complex nature of these interactions. The study also found an enhanced probability of rainfall following heatwave, particularly in the eastern regions, drawing attention to the potential for increased flood risks post-heatwave. Our findings contribute to the growing body of knowledge on the impacts of heatwave on hydrological factors, providing valuable insights for climate change adaptation and water resource management strategies.</description><identifier>ISSN: 0022-1694</identifier><identifier>EISSN: 1879-2707</identifier><identifier>DOI: 10.1016/j.jhydrol.2024.131368</identifier><language>eng</language><publisher>United States: Elsevier B.V</publisher><subject>climate change ; Contiguous United States ; drought ; ENVIRONMENTAL SCIENCES ; evapotranspiration ; GLDAS ; groundwater ; heat ; Heatwave events ; Hydrologic Cycle ; Northeastern United States ; probability ; rain ; relative humidity ; rhizosphere ; runoff ; soil water ; Southeastern United States ; temperature ; water management ; water storage</subject><ispartof>Journal of hydrology (Amsterdam), 2024-06, Vol.637, p.131368, Article 131368</ispartof><rights>2024 Elsevier B.V.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c317t-7099329b777be6064c62c7f0530b9a4a9f5df42234f2d220fb7dcbd801bdedfe3</cites><orcidid>0000-0002-2050-7373 ; 0000000220507373</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0022169424007637$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,314,776,780,881,3537,27901,27902,65306</link.rule.ids><backlink>$$Uhttps://www.osti.gov/biblio/2397411$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Hao, Yuefeng</creatorcontrib><creatorcontrib>Mao, Jiafu</creatorcontrib><creatorcontrib>Jin, Mingzhou</creatorcontrib><creatorcontrib>Wang, Yaoping</creatorcontrib><creatorcontrib>Tang, Rongyun</creatorcontrib><creatorcontrib>Lee, Zhe Weng</creatorcontrib><creatorcontrib>Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)</creatorcontrib><title>Evaluating the effects of heatwave events on hydrological processes in the contiguous United States (2003–2022)</title><title>Journal of hydrology (Amsterdam)</title><description>•Rainfall leads to increased humidity and a subsequent end to the heatwave.•Post- heatwave periods witness a notable decrease in water storage.•Heatwave conclusions correspond with heightened rainfall and increased runoff.•Rainfall is more probable post- heatwave than in non– heatwave intervals.
Extreme heat and drought conditions are affecting water availability in many regions worldwide, leading to negative impacts on human societies, agriculture, and ecosystems. However, current research lacks comprehensive spatiotemporal analysis examining the interplay between multiple hydrological factors and heatwave events, especially in the context of climate change. This research broadly pertains to understanding the dynamics of hydrological factors and their potential responses to heatwave during warm seasons across the contiguous United States for the period from 2003 to 2022. Utilizing data from the Global Land Data Assimilation System (GLDAS), we analyzed surface runoff, evapotranspiration (ET), precipitation, Groundwater Storage (GWS), Root Zone Soil Moisture (RZSM), and Total Water Storage (TWS) to discern annual patterns and the impacts of heatwave. The spatial patterns of heatwave highlighted a higher occurrence in the western, central, and northeastern U.S., with longer average durations in the western and south-central regions. These events are predominantly dry, characterized by low Relative Humidity (RH), except in the southeastern U.S., where heatwave coincide with high RH levels. Post-heatwave analysis indicated a reduction in GWS, TWS, RZSM, and ET, alongside an increase in surface runoff, RH, and precipitation. An in-depth examination of rainfall and temperature dynamics during heatwave revealed weak correlations between rainfall and temperature, as well as between rainfall and heatwave duration, highlighting the complex nature of these interactions. The study also found an enhanced probability of rainfall following heatwave, particularly in the eastern regions, drawing attention to the potential for increased flood risks post-heatwave. Our findings contribute to the growing body of knowledge on the impacts of heatwave on hydrological factors, providing valuable insights for climate change adaptation and water resource management strategies.</description><subject>climate change</subject><subject>Contiguous United States</subject><subject>drought</subject><subject>ENVIRONMENTAL SCIENCES</subject><subject>evapotranspiration</subject><subject>GLDAS</subject><subject>groundwater</subject><subject>heat</subject><subject>Heatwave events</subject><subject>Hydrologic Cycle</subject><subject>Northeastern United States</subject><subject>probability</subject><subject>rain</subject><subject>relative humidity</subject><subject>rhizosphere</subject><subject>runoff</subject><subject>soil water</subject><subject>Southeastern United States</subject><subject>temperature</subject><subject>water management</subject><subject>water storage</subject><issn>0022-1694</issn><issn>1879-2707</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNqFUctOwzAQtBBIlMcnIFmcyiHFjzRuTgih8pCQOABny7HXratg09gt6o1_4A_5EhzCnb2stDuzO6NB6IySCSW0ulxNVsud6UI7YYSVE8opr2Z7aERnoi6YIGIfjQhhrKBVXR6ioxhXJBfn5Qit51vVblRyfoHTEjBYCzpFHCxegkofaptnW_D9yOPhTVg4rVr83gUNMULEzv9ydfDJLTZhE_GrdwkMfk4q5f2Y5W_fn19ZHrs4QQdWtRFO__oxer2dv9zcF49Pdw8314-F5lSkQpC65qxuhBANVKQqdcW0sGTKSVOrUtV2amzJGC8tM4wR2wijGzMjtDFgLPBjdD7cDTE5GXUWpJdZos_-JOO1KCnNoPEAymbWG4hJvrmooW2Vh-xDcjrlglYzQTJ0OkB1F2LswMr3zr2pbicpkX0OciX_cpB9DnLIIfOuBh5ks1sHXa8FvAbjul6KCe6fCz8W1pSQ</recordid><startdate>20240601</startdate><enddate>20240601</enddate><creator>Hao, Yuefeng</creator><creator>Mao, Jiafu</creator><creator>Jin, Mingzhou</creator><creator>Wang, Yaoping</creator><creator>Tang, Rongyun</creator><creator>Lee, Zhe Weng</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7S9</scope><scope>L.6</scope><scope>OTOTI</scope><orcidid>https://orcid.org/0000-0002-2050-7373</orcidid><orcidid>https://orcid.org/0000000220507373</orcidid></search><sort><creationdate>20240601</creationdate><title>Evaluating the effects of heatwave events on hydrological processes in the contiguous United States (2003–2022)</title><author>Hao, Yuefeng ; Mao, Jiafu ; Jin, Mingzhou ; Wang, Yaoping ; Tang, Rongyun ; Lee, Zhe Weng</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c317t-7099329b777be6064c62c7f0530b9a4a9f5df42234f2d220fb7dcbd801bdedfe3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>climate change</topic><topic>Contiguous United States</topic><topic>drought</topic><topic>ENVIRONMENTAL SCIENCES</topic><topic>evapotranspiration</topic><topic>GLDAS</topic><topic>groundwater</topic><topic>heat</topic><topic>Heatwave events</topic><topic>Hydrologic Cycle</topic><topic>Northeastern United States</topic><topic>probability</topic><topic>rain</topic><topic>relative humidity</topic><topic>rhizosphere</topic><topic>runoff</topic><topic>soil water</topic><topic>Southeastern United States</topic><topic>temperature</topic><topic>water management</topic><topic>water storage</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hao, Yuefeng</creatorcontrib><creatorcontrib>Mao, Jiafu</creatorcontrib><creatorcontrib>Jin, Mingzhou</creatorcontrib><creatorcontrib>Wang, Yaoping</creatorcontrib><creatorcontrib>Tang, Rongyun</creatorcontrib><creatorcontrib>Lee, Zhe Weng</creatorcontrib><creatorcontrib>Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)</creatorcontrib><collection>CrossRef</collection><collection>AGRICOLA</collection><collection>AGRICOLA - Academic</collection><collection>OSTI.GOV</collection><jtitle>Journal of hydrology (Amsterdam)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hao, Yuefeng</au><au>Mao, Jiafu</au><au>Jin, Mingzhou</au><au>Wang, Yaoping</au><au>Tang, Rongyun</au><au>Lee, Zhe Weng</au><aucorp>Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)</aucorp><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Evaluating the effects of heatwave events on hydrological processes in the contiguous United States (2003–2022)</atitle><jtitle>Journal of hydrology (Amsterdam)</jtitle><date>2024-06-01</date><risdate>2024</risdate><volume>637</volume><spage>131368</spage><pages>131368-</pages><artnum>131368</artnum><issn>0022-1694</issn><eissn>1879-2707</eissn><abstract>•Rainfall leads to increased humidity and a subsequent end to the heatwave.•Post- heatwave periods witness a notable decrease in water storage.•Heatwave conclusions correspond with heightened rainfall and increased runoff.•Rainfall is more probable post- heatwave than in non– heatwave intervals.
Extreme heat and drought conditions are affecting water availability in many regions worldwide, leading to negative impacts on human societies, agriculture, and ecosystems. However, current research lacks comprehensive spatiotemporal analysis examining the interplay between multiple hydrological factors and heatwave events, especially in the context of climate change. This research broadly pertains to understanding the dynamics of hydrological factors and their potential responses to heatwave during warm seasons across the contiguous United States for the period from 2003 to 2022. Utilizing data from the Global Land Data Assimilation System (GLDAS), we analyzed surface runoff, evapotranspiration (ET), precipitation, Groundwater Storage (GWS), Root Zone Soil Moisture (RZSM), and Total Water Storage (TWS) to discern annual patterns and the impacts of heatwave. The spatial patterns of heatwave highlighted a higher occurrence in the western, central, and northeastern U.S., with longer average durations in the western and south-central regions. These events are predominantly dry, characterized by low Relative Humidity (RH), except in the southeastern U.S., where heatwave coincide with high RH levels. Post-heatwave analysis indicated a reduction in GWS, TWS, RZSM, and ET, alongside an increase in surface runoff, RH, and precipitation. An in-depth examination of rainfall and temperature dynamics during heatwave revealed weak correlations between rainfall and temperature, as well as between rainfall and heatwave duration, highlighting the complex nature of these interactions. The study also found an enhanced probability of rainfall following heatwave, particularly in the eastern regions, drawing attention to the potential for increased flood risks post-heatwave. Our findings contribute to the growing body of knowledge on the impacts of heatwave on hydrological factors, providing valuable insights for climate change adaptation and water resource management strategies.</abstract><cop>United States</cop><pub>Elsevier B.V</pub><doi>10.1016/j.jhydrol.2024.131368</doi><orcidid>https://orcid.org/0000-0002-2050-7373</orcidid><orcidid>https://orcid.org/0000000220507373</orcidid></addata></record> |
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subjects | climate change Contiguous United States drought ENVIRONMENTAL SCIENCES evapotranspiration GLDAS groundwater heat Heatwave events Hydrologic Cycle Northeastern United States probability rain relative humidity rhizosphere runoff soil water Southeastern United States temperature water management water storage |
title | Evaluating the effects of heatwave events on hydrological processes in the contiguous United States (2003–2022) |
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