Precipitation response to extreme soil moisture conditions over the Mediterranean

Abstract The intimate link between soil moisture and precipitation makes it a “chicken-and-egg situation” that challenges climate studies of the continental water cycle. This association is particularly acute over the Mediterranean, increasingly exposed to droughts with climate change. This study ai...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Ardilouze, Constantin [verfasserIn] Materia, Stefano Batté, Lauriane Benassi, Marianna Prodhomme, Chloé

Format:	Artikel
Sprache:	Englisch

Erschienen:	2020

Schlagwörter:	Soil moisture Precipitation Mediterranean Land-atmosphere coupling

Anmerkung:	© The Author(s) 2020

Übergeordnetes Werk:	Enthalten in: Climate dynamics - Springer Berlin Heidelberg, 1986, 58(2020), 7-8 vom: 13. Nov., Seite 1927-1942
Übergeordnetes Werk:	volume:58 ; year:2020 ; number:7-8 ; day:13 ; month:11 ; pages:1927-1942

Links:	Volltext

DOI / URN:	10.1007/s00382-020-05519-5

Katalog-ID:	OLC2078477567

Internformat


LEADER	01000caa a22002652 4500
001	OLC2078477567
003	DE-627
005	20230506010025.0
007	tu
008	221220s2020 xx \|\|\|\|\| 00\| \|\|eng c
024	7		\|a 10.1007/s00382-020-05519-5 \|2 doi
035			\|a (DE-627)OLC2078477567
035			\|a (DE-He213)s00382-020-05519-5-p
040			\|a DE-627 \|b ger \|c DE-627 \|e rakwb
041			\|a eng
082	0	4	\|a 550 \|q VZ
082	0	4	\|a 550 \|q VZ
084			\|a 16,13 \|2 ssgn
100	1		\|a Ardilouze, Constantin \|e verfasserin \|0 (orcid)0000-0003-3949-4450 \|4 aut
245	1	0	\|a Precipitation response to extreme soil moisture conditions over the Mediterranean
264		1	\|c 2020
336			\|a Text \|b txt \|2 rdacontent
337			\|a ohne Hilfsmittel zu benutzen \|b n \|2 rdamedia
338			\|a Band \|b nc \|2 rdacarrier
500			\|a © The Author(s) 2020
520			\|a Abstract The intimate link between soil moisture and precipitation makes it a “chicken-and-egg situation” that challenges climate studies of the continental water cycle. This association is particularly acute over the Mediterranean, increasingly exposed to droughts with climate change. This study aims at deciphering the impact of spring soil moisture state in the Mediterranean on subsequent warm season precipitation. In an idealized setup, two distinct climate models are used to generate extreme dry or wet soil conditions, and run climate simulations initialized and/or forced by these conditions. Changes in precipitation distribution and persistence are analyzed and where applicable compared to composites from a reanalysis. Spring soil moisture anomalies are found to be very persistent, but the precipitation response is largely model dependent. Overall, dry soils lead to a reduction of precipitation for early summer months and conversely for wet soils although with a fainter and less robust signal. On the other hand, wet soils tend to favor the persistence of precipitation throughout summer over several sub-regions. Our results highlight the stringent need to reduce the wide array of uncertainties associated to soil moisture, land-atmosphere coupling and convection in climate models, before ascertaining that soil moisture initialization could provide more skillful sub-seasonal to seasonal precipitation prediction.
650		4	\|a Soil moisture
650		4	\|a Precipitation
650		4	\|a Mediterranean
650		4	\|a Land-atmosphere coupling
700	1		\|a Materia, Stefano \|4 aut
700	1		\|a Batté, Lauriane \|4 aut
700	1		\|a Benassi, Marianna \|4 aut
700	1		\|a Prodhomme, Chloé \|4 aut
773	0	8	\|i Enthalten in \|t Climate dynamics \|d Springer Berlin Heidelberg, 1986 \|g 58(2020), 7-8 vom: 13. Nov., Seite 1927-1942 \|w (DE-627)129932728 \|w (DE-600)382992-3 \|w (DE-576)015479005 \|x 0930-7575 \|7 nnns
773	1	8	\|g volume:58 \|g year:2020 \|g number:7-8 \|g day:13 \|g month:11 \|g pages:1927-1942
856	4	1	\|u https://doi.org/10.1007/s00382-020-05519-5 \|z lizenzpflichtig \|3 Volltext
912			\|a GBV_USEFLAG_A
912			\|a SYSFLAG_A
912			\|a GBV_OLC
912			\|a SSG-OLC-GEO
912			\|a SSG-OPC-GGO
912			\|a SSG-OPC-GEO
912			\|a GBV_ILN_62
912			\|a GBV_ILN_154
912			\|a GBV_ILN_2018
912			\|a GBV_ILN_4277
951			\|a AR
952			\|d 58 \|j 2020 \|e 7-8 \|b 13 \|c 11 \|h 1927-1942

Indexfelder

author_variant	c a ca s m sm l b lb m b mb c p cp
matchkey_str	article:09307575:2020----::rcpttorsosteteeolosueodtosv
hierarchy_sort_str	2020
publishDate	2020
allfields	10.1007/s00382-020-05519-5 doi (DE-627)OLC2078477567 (DE-He213)s00382-020-05519-5-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Ardilouze, Constantin verfasserin (orcid)0000-0003-3949-4450 aut Precipitation response to extreme soil moisture conditions over the Mediterranean 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2020 Abstract The intimate link between soil moisture and precipitation makes it a “chicken-and-egg situation” that challenges climate studies of the continental water cycle. This association is particularly acute over the Mediterranean, increasingly exposed to droughts with climate change. This study aims at deciphering the impact of spring soil moisture state in the Mediterranean on subsequent warm season precipitation. In an idealized setup, two distinct climate models are used to generate extreme dry or wet soil conditions, and run climate simulations initialized and/or forced by these conditions. Changes in precipitation distribution and persistence are analyzed and where applicable compared to composites from a reanalysis. Spring soil moisture anomalies are found to be very persistent, but the precipitation response is largely model dependent. Overall, dry soils lead to a reduction of precipitation for early summer months and conversely for wet soils although with a fainter and less robust signal. On the other hand, wet soils tend to favor the persistence of precipitation throughout summer over several sub-regions. Our results highlight the stringent need to reduce the wide array of uncertainties associated to soil moisture, land-atmosphere coupling and convection in climate models, before ascertaining that soil moisture initialization could provide more skillful sub-seasonal to seasonal precipitation prediction. Soil moisture Precipitation Mediterranean Land-atmosphere coupling Materia, Stefano aut Batté, Lauriane aut Benassi, Marianna aut Prodhomme, Chloé aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 58(2020), 7-8 vom: 13. Nov., Seite 1927-1942 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:58 year:2020 number:7-8 day:13 month:11 pages:1927-1942 https://doi.org/10.1007/s00382-020-05519-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 58 2020 7-8 13 11 1927-1942
spelling	10.1007/s00382-020-05519-5 doi (DE-627)OLC2078477567 (DE-He213)s00382-020-05519-5-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Ardilouze, Constantin verfasserin (orcid)0000-0003-3949-4450 aut Precipitation response to extreme soil moisture conditions over the Mediterranean 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2020 Abstract The intimate link between soil moisture and precipitation makes it a “chicken-and-egg situation” that challenges climate studies of the continental water cycle. This association is particularly acute over the Mediterranean, increasingly exposed to droughts with climate change. This study aims at deciphering the impact of spring soil moisture state in the Mediterranean on subsequent warm season precipitation. In an idealized setup, two distinct climate models are used to generate extreme dry or wet soil conditions, and run climate simulations initialized and/or forced by these conditions. Changes in precipitation distribution and persistence are analyzed and where applicable compared to composites from a reanalysis. Spring soil moisture anomalies are found to be very persistent, but the precipitation response is largely model dependent. Overall, dry soils lead to a reduction of precipitation for early summer months and conversely for wet soils although with a fainter and less robust signal. On the other hand, wet soils tend to favor the persistence of precipitation throughout summer over several sub-regions. Our results highlight the stringent need to reduce the wide array of uncertainties associated to soil moisture, land-atmosphere coupling and convection in climate models, before ascertaining that soil moisture initialization could provide more skillful sub-seasonal to seasonal precipitation prediction. Soil moisture Precipitation Mediterranean Land-atmosphere coupling Materia, Stefano aut Batté, Lauriane aut Benassi, Marianna aut Prodhomme, Chloé aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 58(2020), 7-8 vom: 13. Nov., Seite 1927-1942 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:58 year:2020 number:7-8 day:13 month:11 pages:1927-1942 https://doi.org/10.1007/s00382-020-05519-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 58 2020 7-8 13 11 1927-1942
allfields_unstemmed	10.1007/s00382-020-05519-5 doi (DE-627)OLC2078477567 (DE-He213)s00382-020-05519-5-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Ardilouze, Constantin verfasserin (orcid)0000-0003-3949-4450 aut Precipitation response to extreme soil moisture conditions over the Mediterranean 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2020 Abstract The intimate link between soil moisture and precipitation makes it a “chicken-and-egg situation” that challenges climate studies of the continental water cycle. This association is particularly acute over the Mediterranean, increasingly exposed to droughts with climate change. This study aims at deciphering the impact of spring soil moisture state in the Mediterranean on subsequent warm season precipitation. In an idealized setup, two distinct climate models are used to generate extreme dry or wet soil conditions, and run climate simulations initialized and/or forced by these conditions. Changes in precipitation distribution and persistence are analyzed and where applicable compared to composites from a reanalysis. Spring soil moisture anomalies are found to be very persistent, but the precipitation response is largely model dependent. Overall, dry soils lead to a reduction of precipitation for early summer months and conversely for wet soils although with a fainter and less robust signal. On the other hand, wet soils tend to favor the persistence of precipitation throughout summer over several sub-regions. Our results highlight the stringent need to reduce the wide array of uncertainties associated to soil moisture, land-atmosphere coupling and convection in climate models, before ascertaining that soil moisture initialization could provide more skillful sub-seasonal to seasonal precipitation prediction. Soil moisture Precipitation Mediterranean Land-atmosphere coupling Materia, Stefano aut Batté, Lauriane aut Benassi, Marianna aut Prodhomme, Chloé aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 58(2020), 7-8 vom: 13. Nov., Seite 1927-1942 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:58 year:2020 number:7-8 day:13 month:11 pages:1927-1942 https://doi.org/10.1007/s00382-020-05519-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 58 2020 7-8 13 11 1927-1942
allfieldsGer	10.1007/s00382-020-05519-5 doi (DE-627)OLC2078477567 (DE-He213)s00382-020-05519-5-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Ardilouze, Constantin verfasserin (orcid)0000-0003-3949-4450 aut Precipitation response to extreme soil moisture conditions over the Mediterranean 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2020 Abstract The intimate link between soil moisture and precipitation makes it a “chicken-and-egg situation” that challenges climate studies of the continental water cycle. This association is particularly acute over the Mediterranean, increasingly exposed to droughts with climate change. This study aims at deciphering the impact of spring soil moisture state in the Mediterranean on subsequent warm season precipitation. In an idealized setup, two distinct climate models are used to generate extreme dry or wet soil conditions, and run climate simulations initialized and/or forced by these conditions. Changes in precipitation distribution and persistence are analyzed and where applicable compared to composites from a reanalysis. Spring soil moisture anomalies are found to be very persistent, but the precipitation response is largely model dependent. Overall, dry soils lead to a reduction of precipitation for early summer months and conversely for wet soils although with a fainter and less robust signal. On the other hand, wet soils tend to favor the persistence of precipitation throughout summer over several sub-regions. Our results highlight the stringent need to reduce the wide array of uncertainties associated to soil moisture, land-atmosphere coupling and convection in climate models, before ascertaining that soil moisture initialization could provide more skillful sub-seasonal to seasonal precipitation prediction. Soil moisture Precipitation Mediterranean Land-atmosphere coupling Materia, Stefano aut Batté, Lauriane aut Benassi, Marianna aut Prodhomme, Chloé aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 58(2020), 7-8 vom: 13. Nov., Seite 1927-1942 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:58 year:2020 number:7-8 day:13 month:11 pages:1927-1942 https://doi.org/10.1007/s00382-020-05519-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 58 2020 7-8 13 11 1927-1942
allfieldsSound	10.1007/s00382-020-05519-5 doi (DE-627)OLC2078477567 (DE-He213)s00382-020-05519-5-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Ardilouze, Constantin verfasserin (orcid)0000-0003-3949-4450 aut Precipitation response to extreme soil moisture conditions over the Mediterranean 2020 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2020 Abstract The intimate link between soil moisture and precipitation makes it a “chicken-and-egg situation” that challenges climate studies of the continental water cycle. This association is particularly acute over the Mediterranean, increasingly exposed to droughts with climate change. This study aims at deciphering the impact of spring soil moisture state in the Mediterranean on subsequent warm season precipitation. In an idealized setup, two distinct climate models are used to generate extreme dry or wet soil conditions, and run climate simulations initialized and/or forced by these conditions. Changes in precipitation distribution and persistence are analyzed and where applicable compared to composites from a reanalysis. Spring soil moisture anomalies are found to be very persistent, but the precipitation response is largely model dependent. Overall, dry soils lead to a reduction of precipitation for early summer months and conversely for wet soils although with a fainter and less robust signal. On the other hand, wet soils tend to favor the persistence of precipitation throughout summer over several sub-regions. Our results highlight the stringent need to reduce the wide array of uncertainties associated to soil moisture, land-atmosphere coupling and convection in climate models, before ascertaining that soil moisture initialization could provide more skillful sub-seasonal to seasonal precipitation prediction. Soil moisture Precipitation Mediterranean Land-atmosphere coupling Materia, Stefano aut Batté, Lauriane aut Benassi, Marianna aut Prodhomme, Chloé aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 58(2020), 7-8 vom: 13. Nov., Seite 1927-1942 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:58 year:2020 number:7-8 day:13 month:11 pages:1927-1942 https://doi.org/10.1007/s00382-020-05519-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 58 2020 7-8 13 11 1927-1942
language	English
source	Enthalten in Climate dynamics 58(2020), 7-8 vom: 13. Nov., Seite 1927-1942 volume:58 year:2020 number:7-8 day:13 month:11 pages:1927-1942
sourceStr	Enthalten in Climate dynamics 58(2020), 7-8 vom: 13. Nov., Seite 1927-1942 volume:58 year:2020 number:7-8 day:13 month:11 pages:1927-1942
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Soil moisture Precipitation Mediterranean Land-atmosphere coupling
dewey-raw	550
isfreeaccess_bool	false
container_title	Climate dynamics
authorswithroles_txt_mv	Ardilouze, Constantin @@aut@@ Materia, Stefano @@aut@@ Batté, Lauriane @@aut@@ Benassi, Marianna @@aut@@ Prodhomme, Chloé @@aut@@
publishDateDaySort_date	2020-11-13T00:00:00Z
hierarchy_top_id	129932728
dewey-sort	3550
id	OLC2078477567
language_de	englisch
fullrecord	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2078477567</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230506010025.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">221220s2020 xx \|\|\|\|\| 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00382-020-05519-5</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2078477567</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s00382-020-05519-5-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">16,13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Ardilouze, Constantin</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0003-3949-4450</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Precipitation response to extreme soil moisture conditions over the Mediterranean</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2020</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© The Author(s) 2020</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The intimate link between soil moisture and precipitation makes it a “chicken-and-egg situation” that challenges climate studies of the continental water cycle. This association is particularly acute over the Mediterranean, increasingly exposed to droughts with climate change. This study aims at deciphering the impact of spring soil moisture state in the Mediterranean on subsequent warm season precipitation. In an idealized setup, two distinct climate models are used to generate extreme dry or wet soil conditions, and run climate simulations initialized and/or forced by these conditions. Changes in precipitation distribution and persistence are analyzed and where applicable compared to composites from a reanalysis. Spring soil moisture anomalies are found to be very persistent, but the precipitation response is largely model dependent. Overall, dry soils lead to a reduction of precipitation for early summer months and conversely for wet soils although with a fainter and less robust signal. On the other hand, wet soils tend to favor the persistence of precipitation throughout summer over several sub-regions. Our results highlight the stringent need to reduce the wide array of uncertainties associated to soil moisture, land-atmosphere coupling and convection in climate models, before ascertaining that soil moisture initialization could provide more skillful sub-seasonal to seasonal precipitation prediction.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Soil moisture</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Precipitation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mediterranean</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Land-atmosphere coupling</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Materia, Stefano</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Batté, Lauriane</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Benassi, Marianna</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Prodhomme, Chloé</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Climate dynamics</subfield><subfield code="d">Springer Berlin Heidelberg, 1986</subfield><subfield code="g">58(2020), 7-8 vom: 13. Nov., Seite 1927-1942</subfield><subfield code="w">(DE-627)129932728</subfield><subfield code="w">(DE-600)382992-3</subfield><subfield code="w">(DE-576)015479005</subfield><subfield code="x">0930-7575</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:58</subfield><subfield code="g">year:2020</subfield><subfield code="g">number:7-8</subfield><subfield code="g">day:13</subfield><subfield code="g">month:11</subfield><subfield code="g">pages:1927-1942</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s00382-020-05519-5</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_154</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4277</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">58</subfield><subfield code="j">2020</subfield><subfield code="e">7-8</subfield><subfield code="b">13</subfield><subfield code="c">11</subfield><subfield code="h">1927-1942</subfield></datafield></record></collection>
author	Ardilouze, Constantin
spellingShingle	Ardilouze, Constantin ddc 550 ssgn 16,13 misc Soil moisture misc Precipitation misc Mediterranean misc Land-atmosphere coupling Precipitation response to extreme soil moisture conditions over the Mediterranean
authorStr	Ardilouze, Constantin
ppnlink_with_tag_str_mv	@@773@@(DE-627)129932728
format	Article
dewey-ones	550 - Earth sciences
delete_txt_mv	keep
author_role	aut aut aut aut aut
collection	OLC
remote_str	false
illustrated	Not Illustrated
issn	0930-7575
topic_title	550 VZ 16,13 ssgn Precipitation response to extreme soil moisture conditions over the Mediterranean Soil moisture Precipitation Mediterranean Land-atmosphere coupling
topic	ddc 550 ssgn 16,13 misc Soil moisture misc Precipitation misc Mediterranean misc Land-atmosphere coupling
topic_unstemmed	ddc 550 ssgn 16,13 misc Soil moisture misc Precipitation misc Mediterranean misc Land-atmosphere coupling
topic_browse	ddc 550 ssgn 16,13 misc Soil moisture misc Precipitation misc Mediterranean misc Land-atmosphere coupling
format_facet	Aufsätze Gedruckte Aufsätze
format_main_str_mv	Text Zeitschrift/Artikel
carriertype_str_mv	nc
hierarchy_parent_title	Climate dynamics
hierarchy_parent_id	129932728
dewey-tens	550 - Earth sciences & geology
hierarchy_top_title	Climate dynamics
isfreeaccess_txt	false
familylinks_str_mv	(DE-627)129932728 (DE-600)382992-3 (DE-576)015479005
title	Precipitation response to extreme soil moisture conditions over the Mediterranean
ctrlnum	(DE-627)OLC2078477567 (DE-He213)s00382-020-05519-5-p
title_full	Precipitation response to extreme soil moisture conditions over the Mediterranean
author_sort	Ardilouze, Constantin
journal	Climate dynamics
journalStr	Climate dynamics
lang_code	eng
isOA_bool	false
dewey-hundreds	500 - Science
recordtype	marc
publishDateSort	2020
contenttype_str_mv	txt
container_start_page	1927
author_browse	Ardilouze, Constantin Materia, Stefano Batté, Lauriane Benassi, Marianna Prodhomme, Chloé
container_volume	58
class	550 VZ 16,13 ssgn
format_se	Aufsätze
author-letter	Ardilouze, Constantin
doi_str_mv	10.1007/s00382-020-05519-5
normlink	(ORCID)0000-0003-3949-4450
normlink_prefix_str_mv	(orcid)0000-0003-3949-4450
dewey-full	550
title_sort	precipitation response to extreme soil moisture conditions over the mediterranean
title_auth	Precipitation response to extreme soil moisture conditions over the Mediterranean
abstract	Abstract The intimate link between soil moisture and precipitation makes it a “chicken-and-egg situation” that challenges climate studies of the continental water cycle. This association is particularly acute over the Mediterranean, increasingly exposed to droughts with climate change. This study aims at deciphering the impact of spring soil moisture state in the Mediterranean on subsequent warm season precipitation. In an idealized setup, two distinct climate models are used to generate extreme dry or wet soil conditions, and run climate simulations initialized and/or forced by these conditions. Changes in precipitation distribution and persistence are analyzed and where applicable compared to composites from a reanalysis. Spring soil moisture anomalies are found to be very persistent, but the precipitation response is largely model dependent. Overall, dry soils lead to a reduction of precipitation for early summer months and conversely for wet soils although with a fainter and less robust signal. On the other hand, wet soils tend to favor the persistence of precipitation throughout summer over several sub-regions. Our results highlight the stringent need to reduce the wide array of uncertainties associated to soil moisture, land-atmosphere coupling and convection in climate models, before ascertaining that soil moisture initialization could provide more skillful sub-seasonal to seasonal precipitation prediction. © The Author(s) 2020
abstractGer	Abstract The intimate link between soil moisture and precipitation makes it a “chicken-and-egg situation” that challenges climate studies of the continental water cycle. This association is particularly acute over the Mediterranean, increasingly exposed to droughts with climate change. This study aims at deciphering the impact of spring soil moisture state in the Mediterranean on subsequent warm season precipitation. In an idealized setup, two distinct climate models are used to generate extreme dry or wet soil conditions, and run climate simulations initialized and/or forced by these conditions. Changes in precipitation distribution and persistence are analyzed and where applicable compared to composites from a reanalysis. Spring soil moisture anomalies are found to be very persistent, but the precipitation response is largely model dependent. Overall, dry soils lead to a reduction of precipitation for early summer months and conversely for wet soils although with a fainter and less robust signal. On the other hand, wet soils tend to favor the persistence of precipitation throughout summer over several sub-regions. Our results highlight the stringent need to reduce the wide array of uncertainties associated to soil moisture, land-atmosphere coupling and convection in climate models, before ascertaining that soil moisture initialization could provide more skillful sub-seasonal to seasonal precipitation prediction. © The Author(s) 2020
abstract_unstemmed	Abstract The intimate link between soil moisture and precipitation makes it a “chicken-and-egg situation” that challenges climate studies of the continental water cycle. This association is particularly acute over the Mediterranean, increasingly exposed to droughts with climate change. This study aims at deciphering the impact of spring soil moisture state in the Mediterranean on subsequent warm season precipitation. In an idealized setup, two distinct climate models are used to generate extreme dry or wet soil conditions, and run climate simulations initialized and/or forced by these conditions. Changes in precipitation distribution and persistence are analyzed and where applicable compared to composites from a reanalysis. Spring soil moisture anomalies are found to be very persistent, but the precipitation response is largely model dependent. Overall, dry soils lead to a reduction of precipitation for early summer months and conversely for wet soils although with a fainter and less robust signal. On the other hand, wet soils tend to favor the persistence of precipitation throughout summer over several sub-regions. Our results highlight the stringent need to reduce the wide array of uncertainties associated to soil moisture, land-atmosphere coupling and convection in climate models, before ascertaining that soil moisture initialization could provide more skillful sub-seasonal to seasonal precipitation prediction. © The Author(s) 2020
collection_details	GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277
container_issue	7-8
title_short	Precipitation response to extreme soil moisture conditions over the Mediterranean
url	https://doi.org/10.1007/s00382-020-05519-5
remote_bool	false
author2	Materia, Stefano Batté, Lauriane Benassi, Marianna Prodhomme, Chloé
author2Str	Materia, Stefano Batté, Lauriane Benassi, Marianna Prodhomme, Chloé
ppnlink	129932728
mediatype_str_mv	n
isOA_txt	false
hochschulschrift_bool	false
doi_str	10.1007/s00382-020-05519-5
up_date	2024-07-03T20:38:14.916Z
_version_	1803591713993785344
fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2078477567</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230506010025.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">221220s2020 xx \|\|\|\|\| 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00382-020-05519-5</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2078477567</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s00382-020-05519-5-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">16,13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Ardilouze, Constantin</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0003-3949-4450</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Precipitation response to extreme soil moisture conditions over the Mediterranean</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2020</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© The Author(s) 2020</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The intimate link between soil moisture and precipitation makes it a “chicken-and-egg situation” that challenges climate studies of the continental water cycle. This association is particularly acute over the Mediterranean, increasingly exposed to droughts with climate change. This study aims at deciphering the impact of spring soil moisture state in the Mediterranean on subsequent warm season precipitation. In an idealized setup, two distinct climate models are used to generate extreme dry or wet soil conditions, and run climate simulations initialized and/or forced by these conditions. Changes in precipitation distribution and persistence are analyzed and where applicable compared to composites from a reanalysis. Spring soil moisture anomalies are found to be very persistent, but the precipitation response is largely model dependent. Overall, dry soils lead to a reduction of precipitation for early summer months and conversely for wet soils although with a fainter and less robust signal. On the other hand, wet soils tend to favor the persistence of precipitation throughout summer over several sub-regions. Our results highlight the stringent need to reduce the wide array of uncertainties associated to soil moisture, land-atmosphere coupling and convection in climate models, before ascertaining that soil moisture initialization could provide more skillful sub-seasonal to seasonal precipitation prediction.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Soil moisture</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Precipitation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mediterranean</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Land-atmosphere coupling</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Materia, Stefano</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Batté, Lauriane</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Benassi, Marianna</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Prodhomme, Chloé</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Climate dynamics</subfield><subfield code="d">Springer Berlin Heidelberg, 1986</subfield><subfield code="g">58(2020), 7-8 vom: 13. Nov., Seite 1927-1942</subfield><subfield code="w">(DE-627)129932728</subfield><subfield code="w">(DE-600)382992-3</subfield><subfield code="w">(DE-576)015479005</subfield><subfield code="x">0930-7575</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:58</subfield><subfield code="g">year:2020</subfield><subfield code="g">number:7-8</subfield><subfield code="g">day:13</subfield><subfield code="g">month:11</subfield><subfield code="g">pages:1927-1942</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s00382-020-05519-5</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_154</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4277</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">58</subfield><subfield code="j">2020</subfield><subfield code="e">7-8</subfield><subfield code="b">13</subfield><subfield code="c">11</subfield><subfield code="h">1927-1942</subfield></datafield></record></collection>
score	7.3986673

Nicht das Richtige dabei?

Schreiben Sie uns!

Precipitation response to extreme soil moisture conditions over the Mediterranean

Nicht das Richtige dabei?

Zugang & Verfügbarkeit

Vorhandene Bände

Nicht das Richtige dabei?