Evaporation enhancement drives the European water-budget deficit during multi-year droughts
In a warming climate, periods with lower than average precipitation will increase in frequency and intensity. During such periods, known as meteorological droughts, the decline in annual runoff may be proportionally larger than the corresponding decline in precipitation. Reasons behind this exacerba...
Saved in:
Published in | Hydrology and earth system sciences Vol. 26; no. 6; pp. 1527 - 1543 |
---|---|
Main Authors | , , , , , |
Format | Journal Article |
Language | English |
Published |
Katlenburg-Lindau
Copernicus GmbH
22.03.2022
Copernicus Publications |
Subjects | |
Online Access | Get full text |
Cover
Loading…
Abstract | In a warming climate, periods with lower than average precipitation will increase in frequency and intensity. During such periods, known as meteorological droughts, the decline in annual runoff may be proportionally larger than the corresponding decline in precipitation. Reasons behind this exacerbation of runoff deficit during dry periods remain largely unknown, and this challenges the predictability of when this exacerbation will occur in the future and how intense it will be. In this work, we tested the hypothesis that runoff deficit exacerbation during droughts is a common feature across climates, driven by evaporation enhancement. We relied on multidecadal records of streamflow and precipitation for more than 200 catchment areas across various European climates, which distinctively show the emergence of similar periods of exacerbated runoff deficit identified in previous studies, i.e. runoff deficit on the order of -20 % to -40 % less than what expected from precipitation deficits. The magnitude of this exacerbation is two to three times larger for basins located in dry regions than for basins in wet regions, and is qualitatively correlated with an increase in annual evaporation during droughts, in the order of +11 % and +33 % over basins characterized by energy-limited and water-limited evaporation regimes, respectively. Thus, enhanced atmospheric and vegetation demand for moisture during dry periods induces a nonlinear precipitation-runoff relationship for low-flow regimes, which results in an unexpectedly large decrease in runoff during periods of already low water availability. Forecasting onset, magnitude, and duration of these drops in runoff have paramount societal and ecological implications, especially in a warming climate, given their supporting role for safeguarding water, food, and energy. The outcome that water basins are prone to this exacerbation of runoff deficit for various climates and evaporation regimes makes further understanding of its patterns of predictability an urgent priority for water-resource planning and management in a warming and drier climate. |
---|---|
AbstractList | In a warming climate, periods with lower than average precipitation will increase in frequency and intensity. During such periods, known as meteorological droughts, the decline in annual runoff may be proportionally larger than the corresponding decline in precipitation. Reasons behind this exacerbation of runoff deficit during dry periods remain largely unknown, and this challenges the predictability of when this exacerbation will occur in the future and how intense it will be. In this work, we tested the hypothesis that runoff deficit exacerbation during droughts is a common feature across climates, driven by evaporation enhancement. We relied on multidecadal records of streamflow and precipitation for more than 200 catchment areas across various European climates, which distinctively show the emergence of similar periods of exacerbated runoff deficit identified in previous studies, i.e. runoff deficit on the order of -20 % to -40 % less than what expected from precipitation deficits. The magnitude of this exacerbation is two to three times larger for basins located in dry regions than for basins in wet regions, and is qualitatively correlated with an increase in annual evaporation during droughts, in the order of +11 % and +33 % over basins characterized by energy-limited and water-limited evaporation regimes, respectively. Thus, enhanced atmospheric and vegetation demand for moisture during dry periods induces a nonlinear precipitation-runoff relationship for low-flow regimes, which results in an unexpectedly large decrease in runoff during periods of already low water availability. Forecasting onset, magnitude, and duration of these drops in runoff have paramount societal and ecological implications, especially in a warming climate, given their supporting role for safeguarding water, food, and energy. The outcome that water basins are prone to this exacerbation of runoff deficit for various climates and evaporation regimes makes further understanding of its patterns of predictability an urgent priority for water-resource planning and management in a warming and drier climate. In a warming climate, periods with lower than average precipitation will increase in frequency and intensity. During such periods, known as meteorological droughts, the decline in annual runoff may be proportionally larger than the corresponding decline in precipitation. Reasons behind this exacerbation of runoff deficit during dry periods remain largely unknown, and this challenges the predictability of when this exacerbation will occur in the future and how intense it will be. In this work, we tested the hypothesis that runoff deficit exacerbation during droughts is a common feature across climates, driven by evaporation enhancement. We relied on multidecadal records of streamflow and precipitation for more than 200 catchment areas across various European climates, which distinctively show the emergence of similar periods of exacerbated runoff deficit identified in previous studies, i.e. runoff deficit on the order of −20 % to −40 % less than what expected from precipitation deficits. The magnitude of this exacerbation is two to three times larger for basins located in dry regions than for basins in wet regions, and is qualitatively correlated with an increase in annual evaporation during droughts, in the order of +11 % and +33 % over basins characterized by energy-limited and water-limited evaporation regimes, respectively. Thus, enhanced atmospheric and vegetation demand for moisture during dry periods induces a nonlinear precipitation-runoff relationship for low-flow regimes, which results in an unexpectedly large decrease in runoff during periods of already low water availability. Forecasting onset, magnitude, and duration of these drops in runoff have paramount societal and ecological implications, especially in a warming climate, given their supporting role for safeguarding water, food, and energy. The outcome that water basins are prone to this exacerbation of runoff deficit for various climates and evaporation regimes makes further understanding of its patterns of predictability an urgent priority for water-resource planning and management in a warming and drier climate. In a warming climate, periods with lower than average precipitation will increase in frequency and intensity. During such periods, known as meteorological droughts, the decline in annual runoff may be proportionally larger than the corresponding decline in precipitation. Reasons behind this exacerbation of runoff deficit during dry periods remain largely unknown, and this challenges the predictability of when this exacerbation will occur in the future and how intense it will be. In this work, we tested the hypothesis that runoff deficit exacerbation during droughts is a common feature across climates, driven by evaporation enhancement. We relied on multidecadal records of streamflow and precipitation for more than 200 catchment areas across various European climates, which distinctively show the emergence of similar periods of exacerbated runoff deficit identified in previous studies, i.e. runoff deficit on the order of −20 % to −40 % less than what expected from precipitation deficits. The magnitude of this exacerbation is two to three times larger for basins located in dry regions than for basins in wet regions, and is qualitatively correlated with an increase in annual evaporation during droughts, in the order of +11 % and +33 % over basins characterized by energy-limited and water-limited evaporation regimes, respectively. Thus, enhanced atmospheric and vegetation demand for moisture during dry periods induces a nonlinear precipitation-runoff relationship for low-flow regimes, which results in an unexpectedly large decrease in runoff during periods of already low water availability. Forecasting onset, magnitude, and duration of these drops in runoff have paramount societal and ecological implications, especially in a warming climate, given their supporting role for safeguarding water, food, and energy. The outcome that water basins are prone to this exacerbation of runoff deficit for various climates and evaporation regimes makes further understanding of its patterns of predictability an urgent priority for water-resource planning and management in a warming and drier climate. |
Audience | Academic |
Author | Camici, Stefania Penna, Daniele Massari, Christian Gabellani, Simone Bruno, Giulia Avanzi, Francesco |
Author_xml | – sequence: 1 fullname: Massari, Christian – sequence: 2 fullname: Avanzi, Francesco – sequence: 3 fullname: Bruno, Giulia – sequence: 4 fullname: Gabellani, Simone – sequence: 5 fullname: Penna, Daniele – sequence: 6 fullname: Camici, Stefania |
BookMark | eNptklFrHCEQx6Wk0OTaD9C3hT71YVN1XV0fQ7imB4FCkzzlQVx33PO41au6afPt4_ZK24MiODL8_jOj_i_QmQ8eEHpP8GVLJPu0hZRqymvSUlFTTOkrdE44FrWQTXf2z_kNukhphzHtOk7P0eP6SR9C1NkFX4Hfam9gAp-rIbonSFXeQrWeYziA9tUPnSHW_TyMUACwzrgS5-j8WE3zPrv6GXQs0jCP25zeotdW7xO8-x1X6OHz-v76S3379WZzfXVbG9Y1uW4Y7o0VXBjMTaebQfaSM0PLLnQnRGu0xmJJi4GQviVMYEwYKwosMcfNCm2OdYegd-oQ3aTjswraqV-JEEelY3ZmD6ojVNAOl9ewwKzk0nLRNFaafgAwpcsKfTjWOsTwfYaU1S7M0ZfxFeWMNJxhyv5Soy5FnbchR20ml4y64lJ0jMq2LdTlf6iyBpicKf9nXcmfCD6eCAqT4Wce9ZyS2tx9O2XJkTUxpBTB_rk4wWqxhFosUYZWiyXUYonmBXIGqV8 |
CitedBy_id | crossref_primary_10_1016_j_jhydrol_2023_130105 crossref_primary_10_1029_2021WR031845 crossref_primary_10_5194_hess_26_6073_2022 crossref_primary_10_1016_j_jhydrol_2024_130707 crossref_primary_10_1016_j_jhydrol_2023_130210 crossref_primary_10_1038_s43247_024_01222_z crossref_primary_10_5194_hess_27_1151_2023 crossref_primary_10_1016_j_atmosres_2023_106856 crossref_primary_10_1016_j_jhydrol_2024_131642 crossref_primary_10_17721_2306_5680_2023_4_2 crossref_primary_10_1029_2022WR033449 crossref_primary_10_1016_j_advwatres_2022_104305 crossref_primary_10_1029_2022WR033538 crossref_primary_10_1016_j_agwat_2024_108735 crossref_primary_10_1016_j_agwat_2024_108878 crossref_primary_10_1029_2022GL100505 crossref_primary_10_1016_j_jhydrol_2024_131023 crossref_primary_10_1029_2022WR032871 crossref_primary_10_1016_j_scitotenv_2024_170249 crossref_primary_10_3390_rs14236091 |
Cites_doi | 10.1029/2020EF001502 10.1002/2015WR017032 10.1016/j.jhydrol.2005.08.004 10.1038/s41558-018-0138-5 10.1016/j.jhydrol.2018.11.026 10.1016/j.ejrh.2015.01.001 10.5194/hess-14-2367-2010 10.1038/s41561-019-0388-5 10.1256/wea.73.04 10.3832/ifor2317-010 10.1016/j.earscirev.2011.01.006 10.5194/gmd-13-4159-2020 10.1080/02626667.2019.1659509 10.1002/2015WR018068 10.1016/j.scitotenv.2019.134332 10.1029/2020GL090391 10.1007/s10584-015-1570-4 10.1038/s41467-020-19924-1 10.1016/j.jhydrol.2018.08.015 10.1038/s41586-018-0240-x 10.1038/nclimate2246 10.5194/hess-26-589-2022 10.2166/nh.2012.024 10.1029/2019GL083294 10.1038/s41467-018-06013-7 10.1111/fwb.12789 10.5194/bg-12-7503-2015 10.1029/2020JD034163 10.1073/pnas.1800141115 10.5194/hess-24-581-2020 10.1038/s41598-017-09643-x 10.1038/nature08238 10.1029/2020MS002214 10.1029/2019GL085653 10.1029/2008JD010201 10.5194/hess-24-2687-2020 10.1002/2014WR015348 10.5194/hess-24-4317-2020 10.1029/2019GL084084 10.1111/j.1469-8137.2008.02436.x 10.1007/s00267-012-9928-0 10.1002/eco.2177 10.1175/JHM-D-13-0188.1 10.1002/hyp.8113 10.1002/wrcr.20123 10.1016/j.jhydrol.2014.10.059 10.1029/2017JD028200 10.5194/hess-20-823-2016 10.1002/2014GL062433 10.1016/j.ancene.2021.100309 10.1016/j.earscirev.2010.02.004 10.1016/j.scitotenv.2020.138172 10.1029/2017WR022412 10.1007/s00382-007-0340-z 10.1073/pnas.1712381114 10.3389/fevo.2019.00225 10.5194/hess-21-6307-2017 10.1007/s11160-018-09545-9 10.1038/s41598-018-27464-4 10.1111/j.1749-8198.2010.00341.x 10.3390/w13050669 10.1029/2018MS001500 10.1002/qj.3803 10.1002/2013WR014994 10.1007/s11258-017-0710-5 10.1002/wat2.1523 10.1016/j.geoderma.2016.11.032 10.1111/j.2517-6161.1964.tb00553.x 10.5194/hess-25-429-2021 10.1038/s41561-018-0294-2 10.1038/s41598-017-19007-0 10.1111/nyas.13912 10.1016/j.gloplacha.2016.06.011 10.1002/hyp.13322 10.3354/cr01177 10.1111/nph.15341 10.1002/grl.50495 10.1088/1748-9326/9/4/044001 10.1093/treephys/tps013 10.1038/s41558-019-0676-5 10.5194/hess-23-3631-2019 10.1002/2016WR019525 10.1038/s41586-020-1941-5 10.1016/S0022-1694(01)00421-8 10.1623/hysj.49.1.7.53993 10.1029/2019WR025286 10.1080/02626667.2013.782407 10.1002/wat2.1277 10.1007/s11600-018-0116-3 10.1002/joc.6126 10.1175/2011JHM1351.1 10.1126/science.abd5085 10.1175/JCLI-D-20-0011.1 |
ContentType | Journal Article |
Copyright | COPYRIGHT 2022 Copernicus GmbH 2022. This work is published under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License. |
Copyright_xml | – notice: COPYRIGHT 2022 Copernicus GmbH – notice: 2022. This work is published under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License. |
DBID | AAYXX CITATION ISR 7QH 7TG 7UA 8FD 8FE 8FG ABJCF ABUWG AFKRA ATCPS AZQEC BENPR BFMQW BGLVJ BHPHI BKSAR C1K CCPQU DWQXO F1W FR3 GNUQQ H96 HCIFZ KL. KR7 L.G L6V M7S PATMY PCBAR PIMPY PQEST PQQKQ PQUKI PRINS PTHSS PYCSY DOA |
DOI | 10.5194/hess-26-1527-2022 |
DatabaseName | CrossRef Science In Context Aqualine Meteorological & Geoastrophysical Abstracts Water Resources Abstracts Technology Research Database ProQuest SciTech Collection ProQuest Technology Collection Materials Science & Engineering Collection ProQuest Central (Alumni) ProQuest Central Agricultural & Environmental Science Collection ProQuest Central Essentials ProQuest Central Continental Europe Database Technology Collection Natural Science Collection Earth, Atmospheric & Aquatic Science Collection Environmental Sciences and Pollution Management ProQuest One Community College ProQuest Central ASFA: Aquatic Sciences and Fisheries Abstracts Engineering Research Database ProQuest Central Student Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources SciTech Premium Collection (Proquest) (PQ_SDU_P3) Meteorological & Geoastrophysical Abstracts - Academic Civil Engineering Abstracts Aquatic Science & Fisheries Abstracts (ASFA) Professional ProQuest Engineering Collection Engineering Database Environmental Science Database Earth, Atmospheric & Aquatic Science Database Publicly Available Content Database ProQuest One Academic Eastern Edition (DO NOT USE) ProQuest One Academic ProQuest One Academic UKI Edition ProQuest Central China Engineering Collection Environmental Science Collection DOAJ Directory of Open Access Journals |
DatabaseTitle | CrossRef Publicly Available Content Database Aquatic Science & Fisheries Abstracts (ASFA) Professional ProQuest Central Student Technology Collection Technology Research Database ProQuest Central Essentials ProQuest Central (Alumni Edition) SciTech Premium Collection ProQuest One Community College ProQuest Central China Water Resources Abstracts Environmental Sciences and Pollution Management Earth, Atmospheric & Aquatic Science Collection ProQuest Central ProQuest Engineering Collection Meteorological & Geoastrophysical Abstracts Natural Science Collection ProQuest Central Korea Agricultural & Environmental Science Collection Engineering Collection Civil Engineering Abstracts Engineering Database ProQuest One Academic Eastern Edition Earth, Atmospheric & Aquatic Science Database ProQuest Technology Collection Continental Europe Database ProQuest SciTech Collection Aqualine Environmental Science Collection Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources ProQuest One Academic UKI Edition ASFA: Aquatic Sciences and Fisheries Abstracts Materials Science & Engineering Collection Environmental Science Database Engineering Research Database ProQuest One Academic Meteorological & Geoastrophysical Abstracts - Academic |
DatabaseTitleList | CrossRef Publicly Available Content Database |
Database_xml | – sequence: 1 dbid: DOA name: DOAJ Directory of Open Access Journals url: https://www.doaj.org/ sourceTypes: Open Website – sequence: 2 dbid: 8FG name: ProQuest Technology Collection url: https://search.proquest.com/technologycollection1 sourceTypes: Aggregation Database |
DeliveryMethod | fulltext_linktorsrc |
Discipline | Geography |
EISSN | 1607-7938 |
EndPage | 1543 |
ExternalDocumentID | oai_doaj_org_article_8127280160fe4f969f6733f9cbdeec07 A697842955 10_5194_hess_26_1527_2022 |
GeographicLocations | Alps Europe |
GeographicLocations_xml | – name: Alps – name: Europe |
GroupedDBID | 29I 2WC 3V. 5GY 5VS 7XC 8CJ 8FE 8FG 8FH 8R4 8R5 AAFWJ AAYXX ABJCF ABUWG ACGFO ACIWK ADBBV AENEX AFKRA AFPKN AFRAH AHGZY AIAGR ALMA_UNASSIGNED_HOLDINGS ATCPS BBORY BCNDV BENPR BFMQW BGLVJ BHPHI BKSAR BPHCQ CCPQU CITATION D1J D1K E3Z EBS ECGQY EDH EJD GROUPED_DOAJ GX1 H13 HCIFZ IAO IEA ISR ITC K6- KQ8 L6V L8X LK5 M7R M7S M~E OK1 P2P PATMY PCBAR PIMPY PQQKQ PROAC PTHSS PYCSY Q2X RIG RKB RNS TR2 XSB ~02 ~KM 7QH 7TG 7UA 8FD AZQEC C1K DWQXO F1W FR3 GNUQQ H96 KL. KR7 L.G PQEST PQUKI PRINS |
ID | FETCH-LOGICAL-c483t-340bcf767c06c8a3d9b964c2b967a8775caa073d9b7d11b514700144767090603 |
IEDL.DBID | DOA |
ISSN | 1607-7938 1027-5606 |
IngestDate | Fri Oct 04 13:14:33 EDT 2024 Thu Oct 10 20:04:35 EDT 2024 Thu Feb 22 23:31:45 EST 2024 Sat Dec 16 00:27:14 EST 2023 Thu Aug 01 20:30:22 EDT 2024 Fri Aug 23 01:50:53 EDT 2024 |
IsDoiOpenAccess | true |
IsOpenAccess | true |
IsPeerReviewed | true |
IsScholarly | true |
Issue | 6 |
Language | English |
LinkModel | DirectLink |
MergedId | FETCHMERGED-LOGICAL-c483t-340bcf767c06c8a3d9b964c2b967a8775caa073d9b7d11b514700144767090603 |
ORCID | 0000-0001-6915-0697 0000-0003-4235-2373 0000-0003-0983-1276 |
OpenAccessLink | https://doaj.org/article/8127280160fe4f969f6733f9cbdeec07 |
PQID | 2641364024 |
PQPubID | 105724 |
PageCount | 17 |
ParticipantIDs | doaj_primary_oai_doaj_org_article_8127280160fe4f969f6733f9cbdeec07 proquest_journals_2641364024 gale_infotracmisc_A697842955 gale_infotracacademiconefile_A697842955 gale_incontextgauss_ISR_A697842955 crossref_primary_10_5194_hess_26_1527_2022 |
PublicationCentury | 2000 |
PublicationDate | 2022-03-22 |
PublicationDateYYYYMMDD | 2022-03-22 |
PublicationDate_xml | – month: 03 year: 2022 text: 2022-03-22 day: 22 |
PublicationDecade | 2020 |
PublicationPlace | Katlenburg-Lindau |
PublicationPlace_xml | – name: Katlenburg-Lindau |
PublicationTitle | Hydrology and earth system sciences |
PublicationYear | 2022 |
Publisher | Copernicus GmbH Copernicus Publications |
Publisher_xml | – name: Copernicus GmbH – name: Copernicus Publications |
References | ref57 ref56 ref59 ref58 ref53 ref52 ref55 ref54 ref51 ref50 ref46 ref45 ref48 ref47 ref42 ref41 ref44 ref43 ref49 ref8 ref7 ref9 ref4 ref3 ref6 ref5 ref100 ref101 ref40 ref35 ref34 ref37 ref36 ref31 ref30 ref33 ref32 ref39 ref38 ref24 ref23 ref26 ref25 ref20 ref22 ref21 ref28 ref27 ref29 ref13 ref12 ref15 ref14 ref97 ref96 ref11 ref99 ref10 ref98 ref17 ref16 ref19 ref18 ref93 ref92 ref95 ref94 ref91 ref90 ref89 ref86 ref85 ref88 ref87 ref82 ref81 ref84 ref83 ref80 ref79 ref78 ref75 ref104 ref74 ref105 ref77 ref102 ref76 ref103 ref2 ref1 ref71 ref70 ref73 ref72 ref68 ref67 ref69 ref64 ref63 ref66 ref65 ref60 ref62 ref61 |
References_xml | – ident: ref40 doi: 10.1029/2020EF001502 – ident: ref62 – ident: ref100 doi: 10.1002/2015WR017032 – ident: ref73 doi: 10.1016/j.jhydrol.2005.08.004 – ident: ref84 doi: 10.1038/s41558-018-0138-5 – ident: ref72 doi: 10.1016/j.jhydrol.2018.11.026 – ident: ref92 doi: 10.1016/j.ejrh.2015.01.001 – ident: ref93 doi: 10.5194/hess-14-2367-2010 – ident: ref35 doi: 10.1038/s41561-019-0388-5 – ident: ref28 doi: 10.1256/wea.73.04 – ident: ref34 doi: 10.3832/ifor2317-010 – ident: ref32 doi: 10.1016/j.earscirev.2011.01.006 – ident: ref56 doi: 10.5194/gmd-13-4159-2020 – ident: ref18 doi: 10.1080/02626667.2019.1659509 – ident: ref13 – ident: ref31 doi: 10.1002/2015WR018068 – ident: ref14 doi: 10.1016/j.scitotenv.2019.134332 – ident: ref24 doi: 10.1029/2020GL090391 – ident: ref79 doi: 10.1007/s10584-015-1570-4 – ident: ref87 doi: 10.1038/s41467-020-19924-1 – ident: ref44 – ident: ref97 doi: 10.1016/j.jhydrol.2018.08.015 – ident: ref15 doi: 10.1038/s41586-018-0240-x – ident: ref8 doi: 10.1038/nclimate2246 – ident: ref50 – ident: ref59 doi: 10.5194/hess-26-589-2022 – ident: ref70 doi: 10.2166/nh.2012.024 – ident: ref39 doi: 10.1029/2019GL083294 – ident: ref68 doi: 10.1038/s41467-018-06013-7 – ident: ref19 doi: 10.1111/fwb.12789 – ident: ref20 doi: 10.5194/bg-12-7503-2015 – ident: ref67 doi: 10.1029/2020JD034163 – ident: ref77 doi: 10.1073/pnas.1800141115 – ident: ref16 – ident: ref76 doi: 10.5194/hess-24-581-2020 – ident: ref7 doi: 10.1038/s41598-017-09643-x – ident: ref78 doi: 10.1038/nature08238 – ident: ref53 doi: 10.1029/2020MS002214 – ident: ref27 doi: 10.1029/2019GL085653 – ident: ref42 doi: 10.1029/2008JD010201 – ident: ref57 doi: 10.5194/hess-24-2687-2020 – ident: ref82 doi: 10.1002/2014WR015348 – ident: ref5 doi: 10.5194/hess-24-4317-2020 – ident: ref104 doi: 10.1029/2019GL084084 – ident: ref60 doi: 10.1111/j.1469-8137.2008.02436.x – ident: ref4 doi: 10.1007/s00267-012-9928-0 – ident: ref3 doi: 10.1002/eco.2177 – ident: ref69 doi: 10.1175/JHM-D-13-0188.1 – ident: ref63 doi: 10.1002/hyp.8113 – ident: ref21 doi: 10.1002/wrcr.20123 – ident: ref55 – ident: ref102 doi: 10.1016/j.jhydrol.2014.10.059 – ident: ref17 doi: 10.1029/2017JD028200 – ident: ref64 doi: 10.5194/hess-20-823-2016 – ident: ref38 doi: 10.1002/2014GL062433 – ident: ref71 doi: 10.1016/j.ancene.2021.100309 – ident: ref86 doi: 10.1016/j.earscirev.2010.02.004 – ident: ref98 doi: 10.1016/j.scitotenv.2020.138172 – ident: ref99 doi: 10.1029/2017WR022412 – ident: ref88 doi: 10.1007/s00382-007-0340-z – ident: ref26 doi: 10.1073/pnas.1712381114 – ident: ref1 doi: 10.3389/fevo.2019.00225 – ident: ref33 doi: 10.5194/hess-21-6307-2017 – ident: ref46 – ident: ref52 doi: 10.1007/s11160-018-09545-9 – ident: ref41 doi: 10.1038/s41598-018-27464-4 – ident: ref91 doi: 10.1111/j.1749-8198.2010.00341.x – ident: ref45 doi: 10.3390/w13050669 – ident: ref48 doi: 10.1029/2018MS001500 – ident: ref43 doi: 10.1002/qj.3803 – ident: ref10 doi: 10.1002/2013WR014994 – ident: ref37 – ident: ref89 – ident: ref47 doi: 10.1007/s11258-017-0710-5 – ident: ref29 doi: 10.1002/wat2.1523 – ident: ref81 doi: 10.1016/j.geoderma.2016.11.032 – ident: ref12 doi: 10.1111/j.2517-6161.1964.tb00553.x – ident: ref2 doi: 10.5194/hess-25-429-2021 – ident: ref11 doi: 10.1038/s41561-018-0294-2 – ident: ref6 doi: 10.1038/s41598-017-19007-0 – ident: ref65 doi: 10.1111/nyas.13912 – ident: ref36 doi: 10.1016/j.gloplacha.2016.06.011 – ident: ref80 doi: 10.1002/hyp.13322 – ident: ref54 doi: 10.3354/cr01177 – ident: ref61 doi: 10.1111/nph.15341 – ident: ref95 doi: 10.1002/grl.50495 – ident: ref103 doi: 10.1088/1748-9326/9/4/044001 – ident: ref22 doi: 10.1093/treephys/tps013 – ident: ref58 doi: 10.1038/s41558-019-0676-5 – ident: ref96 doi: 10.5194/hess-23-3631-2019 – ident: ref83 doi: 10.1002/2016WR019525 – ident: ref94 doi: 10.1038/s41586-020-1941-5 – ident: ref9 doi: 10.1016/S0022-1694(01)00421-8 – ident: ref51 doi: 10.1623/hysj.49.1.7.53993 – ident: ref25 – ident: ref101 – ident: ref30 doi: 10.1029/2019WR025286 – ident: ref66 doi: 10.1080/02626667.2013.782407 – ident: ref49 doi: 10.1002/wat2.1277 – ident: ref90 – ident: ref75 doi: 10.1007/s11600-018-0116-3 – ident: ref23 doi: 10.1002/joc.6126 – ident: ref105 doi: 10.1175/2011JHM1351.1 – ident: ref74 doi: 10.1126/science.abd5085 – ident: ref85 doi: 10.1175/JCLI-D-20-0011.1 |
SSID | ssj0028862 |
Score | 2.514405 |
Snippet | In a warming climate, periods with lower than average
precipitation will increase in frequency and intensity. During such periods,
known as meteorological... In a warming climate, periods with lower than average precipitation will increase in frequency and intensity. During such periods, known as meteorological... |
SourceID | doaj proquest gale crossref |
SourceType | Open Website Aggregation Database |
StartPage | 1527 |
SubjectTerms | Annual runoff Basins Budget deficits Catchment area Catchment areas Climate Drought Droughts Dry periods Energy limitation Evaporation Global warming Hydrology Low flow Precipitation Precipitation (Meteorology) Rainfall-runoff relationships Runoff Stream discharge Stream flow Streamflow Vegetation Water Water availability Water resources |
SummonAdditionalLinks | – databaseName: ProQuest Central dbid: BENPR link: http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwfV3dSxwxEA-tPtgX0Vbp1Q8WKRQKwWw2m-w-iSeKCpViKwg-hHzePe1d1z3k_ntn9rLCPdSXXUhmWTKTzPwmk8wQ8j0EbhyTjkZhGBXgQVALyIBWwYrSxQhOB94d_nUnrx_E7WP5mDbcntOxykEn9orazxzukZ-C4c4LCd6OOJv_o1g1CqOrqYTGR7LJc4Fh2s3x5d3v-zeXq6rkKt7JFQXbLldxTUAt4nQKmoRySbGuK8wVztcsU5_A_39qurc9VztkO4HG7Hwl5V3yITSfyVaqXz5dfiFPAIjnSZhZaKYoStz2y3yLaWUzQHnZsO-evQC8bKld-EkAgoApJODdX1fM-vOFdAnTHz7FAj7d8x55uLr8e3FNU9kE6kRVdLQQzLqopEIZVKbwta2lcByeylRKlc4YWNjQrHyeW0BMGHsWQmEqNyZZsU82mlkTvpKMBdAI3ue-MFEwZ63jKvq6NLI0JloxIj8Hlun5KjuGBq8C-auRv5pLjfzVyN8RGSNT3wgxsXXfMGsnOq0TDXgDC2blksUgYi3rKFVRxNpZH4JjakROUCQaU1c0eDZmYhbwn5s_9_pcgkcM5rUsR-RHIoqzrjXOpKsGMCjMdrVGebhGCWvLrXcPktdpbeOYhpn47f3uA_IJx40n1jg_JBtduwhHAGE6e5zm6SslnO7v priority: 102 providerName: ProQuest |
Title | Evaporation enhancement drives the European water-budget deficit during multi-year droughts |
URI | https://www.proquest.com/docview/2641364024 https://doaj.org/article/8127280160fe4f969f6733f9cbdeec07 |
Volume | 26 |
hasFullText | 1 |
inHoldings | 1 |
isFullTextHit | |
isPrint | |
link | http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwrV3NS91AEB9ae7CXUm2lr9pHEKFQWEw2m93kqMXnByjWVhQ8LPvpO0V55iH-984k-0rfQXrxkoVkQrK_2d2Z2Y_fAOyEwI3LpWNRmJwJjCCYRc-A1cGKysWIQQedHT49k0eX4uS6uv4n1RftCRvogQfgdtEAUQalQuYxiNjIJkpVlrFx1ofg0jnyoloEUynUqms5rHNyxdCmy2E9E70VsTvFEYRxySifK7YRzpcsUk_c_9Lw3NucyUf4kJzFbG_4yTV4E9p1WE15y6dPn-AGHeH7pMQstFNSIU33ZX5GdLIZenfZYr49e0S3csbs3N8GFAhEHYFlf0wx6_cVsids9vgqJe7pHj7D5eTgz88jltIlMCfqsmOlyK2LSirCvjalb2wjheN4VaZWqnLGYIfG28oXhUVPidachVBE4ZbLvNyAlfauDV8gywOOBN4XvjRR5M5ax1X0TWVkZUy0YgQ_FpDp-4EVQ2M0QfhqwldzqQlfTfiOYJ9A_StIhNb9DVSzTmrW_1PzCLZJJZooK1raE3Nr5vid498Xek9iJIxmtapG8D0JxbtuZpxJRwywUsRytSS5tSSJfcotP15oXqc-TXVCgy8x3hZfX6NGm_Ce0KH9bJxvwUo3m4dv6OB0dgxv68nhGN7tH5ydX1A5Of11Ne5b-DOHR_of |
link.rule.ids | 315,786,790,870,2115,12792,21416,27955,27956,33406,33777,43633,43838,74390,74657 |
linkProvider | Directory of Open Access Journals |
linkToHtml | http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwfV1La9wwEBZtekguoU-6adqaUigURGRJluxTSUu3mzbJoU0g0IPQc_fk3TpeQv59ZrxyYA_pxQZpjNHMaOYbPWYI-Rgjt54pT5O0jEqIIKgDZEDr6GTlU4KgA-8On52r2aX8eVVd5QW363yscrSJg6EOS49r5EfguEuhINqRX1b_KFaNwt3VXELjMXkihRKo5_X0x33AVddqs9vJNQXPrja7moBZ5NEC7AjlimJVV9AUzrf80pC-_yEjPXie6VOynyFjcbyR8TPyKLbPyW6uXr64fUH-AhxeZVEWsV2gIHHRrwgdJpUtAOMV46p7cQPgsqNuHeYRCCImkID3cFmxGE4X0ltQfvgUy_f01y_J5fT7xbcZzUUTqJe16KmQzPmklUYJ1FaExjVKeg5PbWutK28tTGto1qEsHeAl3HmWUmMiN6aYeEV22mUbX5OCRbAHIZRB2CSZd85znUJTWVVZm5yckM8jy8xqkxvDQEyB_DXIX8OVQf4a5O-EfEWm3hNiWuuhYdnNTZ4lBtAGlssqFUtRpkY1SWkhUuNdiNEzPSEfUCQGE1e0eDJmbtfwn5M_v82xgngYnGtVTcinTJSWfWe9zRcNYFCY62qL8nCLEmaW3-4eJW_yzMYxjXp48P_u92R3dnF2ak5Pzn-9IXvIAzy7xvkh2em7dXwLYKZ37waNvQNyWvB2 |
linkToPdf | http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwfV3dS9xAEF-qhdqXYr_w1GooQqGw3Gaz2U2eilWv2lopbQWhD8t-3j3lrjFH8b_vTG4j3IO-5CCZI2Q-f7M7O0PIUQjcOCYdjcIwKiCDoBaQAa2CFaWLEZIOPDv8_UqeX4uvN-VNqn-6TWWVg0_sHbWfO1wjH0PgzgsJ2Y4Yx1QW8eN08mnxl-IEKdxpTeM0NshTBNk4xqGafLlPvqpKrnY-uaIQ5eVqhxPwixjPwKdQLilOeAWt4XwtRvWt_B9y2H0UmmyTFwk-Zscreb8kT0LzimylSeazu9fkD0DjRRJrFpoZChUXADPfYoPZDPBeNqzAZ_8AaLbULv00AEHAZhLw2x9czPpKQ3oHhgB_xVE-3e0bcj05-31yTtMABepEVXS0EMy6qKRCaVSm8LWtpXAcrspUSpXOGDBxuK18nlvATrgLLYTCpm5MsuIt2WzmTdghGQvgG7zPfWGiYM5ax1X0dWlkaUy0YkQ-DizTi1WfDA35BfJXI381lxr5q5G_I_IZmXpPiC2u-xvzdqqTxWhAHjg6K5csBhFrWUepiiLWzvoQHFMj8h5ForGJRYPqMDVLeM_Fr5_6WEJuDIG2LEfkQyKK8641zqRDB_BR2PdqjXJ_jRKszK0_HiSvk5XjNw06ufv440PyDJRVX15cfdsjz5EFWMbG-T7Z7NpleAe4prMHvcL-B8m_9Ks |
openUrl | ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fsummon.serialssolutions.com&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.atitle=Evaporation+enhancement+drives+the+European+water-budget+deficit+during+multi-year+droughts&rft.jtitle=Hydrology+and+earth+system+sciences&rft.au=Massari%2C+Christian&rft.au=Avanzi%2C+Francesco&rft.au=Bruno%2C+Giulia&rft.au=Gabellani%2C+Simone&rft.date=2022-03-22&rft.pub=Copernicus+GmbH&rft.issn=1027-5606&rft.eissn=1607-7938&rft.volume=26&rft.issue=6&rft.spage=1527&rft_id=info:doi/10.5194%2Fhess-26-1527-2022&rft.externalDocID=A697842955 |
thumbnail_l | http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/lc.gif&issn=1607-7938&client=summon |
thumbnail_m | http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/mc.gif&issn=1607-7938&client=summon |
thumbnail_s | http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/sc.gif&issn=1607-7938&client=summon |