Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan

Hydrological models play a key role in simulating and assessing climate and land use/cover (LULC) change impacts on hydrology in a watershed. In this study, the impact of climate and LULC change was investigated using the Soil and Water Assessment Tool (SWAT) model. The simulated and observed stream...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Jamal Hassan Ougahi [verfasserIn] Shahid Karim [verfasserIn] Syed Amer Mahmood [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2022

Schlagwörter:	climate change kabul river basin land use change swat model water balance components

Übergeordnetes Werk:	In: Journal of Water and Climate Change - IWA Publishing, 2021, 13(2022), 11, Seite 3977-3999
Übergeordnetes Werk:	volume:13 ; year:2022 ; number:11 ; pages:3977-3999

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.2166/wcc.2022.261

Katalog-ID:	DOAJ026400502

Internformat


LEADER	01000caa a22002652 4500
001	DOAJ026400502
003	DE-627
005	20230307101356.0
007	cr uuu---uuuuu
008	230226s2022 xx \|\|\|\|\|o 00\| \|\|eng c
024	7		\|a 10.2166/wcc.2022.261 \|2 doi
035			\|a (DE-627)DOAJ026400502
035			\|a (DE-599)DOAJ5c3e9fcf300c425193d9478fa67425c1
040			\|a DE-627 \|b ger \|c DE-627 \|e rakwb
041			\|a eng
050		0	\|a TD1-1066
050		0	\|a GE1-350
100	0		\|a Jamal Hassan Ougahi \|e verfasserin \|4 aut
245	1	0	\|a Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan
264		1	\|c 2022
336			\|a Text \|b txt \|2 rdacontent
337			\|a Computermedien \|b c \|2 rdamedia
338			\|a Online-Ressource \|b cr \|2 rdacarrier
520			\|a Hydrological models play a key role in simulating and assessing climate and land use/cover (LULC) change impacts on hydrology in a watershed. In this study, the impact of climate and LULC change was investigated using the Soil and Water Assessment Tool (SWAT) model. The simulated and observed streamflow showed a good agreement. Both Nash–Sutcliffe Efficiency (NSE) and coefficient of determination (R2) were found to be greater than 0.7 during the calibration (1985–2002) and validation (2003–2012) period. The water balance components were simulated with inputs from downscaled Global Climate Models (GCMs) data (i.e., future scenario (2030–2100) relative to a baseline period (1974–2004)) under RCP4.5 and RCP8.5, and hypothetical generated LULC change scenarios. All GCMs projected an increase in temperature over the Kabul River Basin (KRB), whereas there was a lack of agreement on projected precipitation among GCMs under both emission and future scenarios. Water yield (WYLD) and evapotranspiration (ET) were projected to decrease in the 21st century. Average annual WYLD was projected to increase under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios. These results are valuable for relevant agencies and stakeholders to adopt measures to counter the negative impacts of climate and LULC change on water resources. HIGHLIGHTS The projected temperature consistently increases in the 21st century.; Most of the GCMs projected a decrease in annual and winter precipitation in the KRB.; The simulated water balance components show a higher impact by climate than LULC change scenarios.; The water yield was increased under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios.;
650		4	\|a climate change
650		4	\|a kabul river basin
650		4	\|a land use change
650		4	\|a swat model
650		4	\|a water balance components
653		0	\|a Environmental technology. Sanitary engineering
653		0	\|a Environmental sciences
700	0		\|a Shahid Karim \|e verfasserin \|4 aut
700	0		\|a Syed Amer Mahmood \|e verfasserin \|4 aut
773	0	8	\|i In \|t Journal of Water and Climate Change \|d IWA Publishing, 2021 \|g 13(2022), 11, Seite 3977-3999 \|w (DE-627)62604703X \|w (DE-600)2552186-X \|x 24089354 \|7 nnns
773	1	8	\|g volume:13 \|g year:2022 \|g number:11 \|g pages:3977-3999
856	4	0	\|u https://doi.org/10.2166/wcc.2022.261 \|z kostenfrei
856	4	0	\|u https://doaj.org/article/5c3e9fcf300c425193d9478fa67425c1 \|z kostenfrei
856	4	0	\|u http://jwcc.iwaponline.com/content/13/11/3977 \|z kostenfrei
856	4	2	\|u https://doaj.org/toc/2040-2244 \|y Journal toc \|z kostenfrei
856	4	2	\|u https://doaj.org/toc/2408-9354 \|y Journal toc \|z kostenfrei
912			\|a GBV_USEFLAG_A
912			\|a SYSFLAG_A
912			\|a GBV_DOAJ
912			\|a GBV_ILN_11
912			\|a GBV_ILN_20
912			\|a GBV_ILN_22
912			\|a GBV_ILN_23
912			\|a GBV_ILN_24
912			\|a GBV_ILN_31
912			\|a GBV_ILN_39
912			\|a GBV_ILN_40
912			\|a GBV_ILN_60
912			\|a GBV_ILN_62
912			\|a GBV_ILN_63
912			\|a GBV_ILN_65
912			\|a GBV_ILN_69
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_95
912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
912			\|a GBV_ILN_151
912			\|a GBV_ILN_161
912			\|a GBV_ILN_170
912			\|a GBV_ILN_213
912			\|a GBV_ILN_230
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_4046
951			\|a AR
952			\|d 13 \|j 2022 \|e 11 \|h 3977-3999

Indexfelder

author_variant	j h o jho s k sk s a m sam
matchkey_str	article:24089354:2022----::plctootewtoetassciaenlnueoecagipcsnaeblneopnn
hierarchy_sort_str	2022
callnumber-subject-code	TD
publishDate	2022
allfields	10.2166/wcc.2022.261 doi (DE-627)DOAJ026400502 (DE-599)DOAJ5c3e9fcf300c425193d9478fa67425c1 DE-627 ger DE-627 rakwb eng TD1-1066 GE1-350 Jamal Hassan Ougahi verfasserin aut Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Hydrological models play a key role in simulating and assessing climate and land use/cover (LULC) change impacts on hydrology in a watershed. In this study, the impact of climate and LULC change was investigated using the Soil and Water Assessment Tool (SWAT) model. The simulated and observed streamflow showed a good agreement. Both Nash–Sutcliffe Efficiency (NSE) and coefficient of determination (R2) were found to be greater than 0.7 during the calibration (1985–2002) and validation (2003–2012) period. The water balance components were simulated with inputs from downscaled Global Climate Models (GCMs) data (i.e., future scenario (2030–2100) relative to a baseline period (1974–2004)) under RCP4.5 and RCP8.5, and hypothetical generated LULC change scenarios. All GCMs projected an increase in temperature over the Kabul River Basin (KRB), whereas there was a lack of agreement on projected precipitation among GCMs under both emission and future scenarios. Water yield (WYLD) and evapotranspiration (ET) were projected to decrease in the 21st century. Average annual WYLD was projected to increase under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios. These results are valuable for relevant agencies and stakeholders to adopt measures to counter the negative impacts of climate and LULC change on water resources. HIGHLIGHTS The projected temperature consistently increases in the 21st century.; Most of the GCMs projected a decrease in annual and winter precipitation in the KRB.; The simulated water balance components show a higher impact by climate than LULC change scenarios.; The water yield was increased under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios.; climate change kabul river basin land use change swat model water balance components Environmental technology. Sanitary engineering Environmental sciences Shahid Karim verfasserin aut Syed Amer Mahmood verfasserin aut In Journal of Water and Climate Change IWA Publishing, 2021 13(2022), 11, Seite 3977-3999 (DE-627)62604703X (DE-600)2552186-X 24089354 nnns volume:13 year:2022 number:11 pages:3977-3999 https://doi.org/10.2166/wcc.2022.261 kostenfrei https://doaj.org/article/5c3e9fcf300c425193d9478fa67425c1 kostenfrei http://jwcc.iwaponline.com/content/13/11/3977 kostenfrei https://doaj.org/toc/2040-2244 Journal toc kostenfrei https://doaj.org/toc/2408-9354 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_4046 AR 13 2022 11 3977-3999
spelling	10.2166/wcc.2022.261 doi (DE-627)DOAJ026400502 (DE-599)DOAJ5c3e9fcf300c425193d9478fa67425c1 DE-627 ger DE-627 rakwb eng TD1-1066 GE1-350 Jamal Hassan Ougahi verfasserin aut Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Hydrological models play a key role in simulating and assessing climate and land use/cover (LULC) change impacts on hydrology in a watershed. In this study, the impact of climate and LULC change was investigated using the Soil and Water Assessment Tool (SWAT) model. The simulated and observed streamflow showed a good agreement. Both Nash–Sutcliffe Efficiency (NSE) and coefficient of determination (R2) were found to be greater than 0.7 during the calibration (1985–2002) and validation (2003–2012) period. The water balance components were simulated with inputs from downscaled Global Climate Models (GCMs) data (i.e., future scenario (2030–2100) relative to a baseline period (1974–2004)) under RCP4.5 and RCP8.5, and hypothetical generated LULC change scenarios. All GCMs projected an increase in temperature over the Kabul River Basin (KRB), whereas there was a lack of agreement on projected precipitation among GCMs under both emission and future scenarios. Water yield (WYLD) and evapotranspiration (ET) were projected to decrease in the 21st century. Average annual WYLD was projected to increase under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios. These results are valuable for relevant agencies and stakeholders to adopt measures to counter the negative impacts of climate and LULC change on water resources. HIGHLIGHTS The projected temperature consistently increases in the 21st century.; Most of the GCMs projected a decrease in annual and winter precipitation in the KRB.; The simulated water balance components show a higher impact by climate than LULC change scenarios.; The water yield was increased under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios.; climate change kabul river basin land use change swat model water balance components Environmental technology. Sanitary engineering Environmental sciences Shahid Karim verfasserin aut Syed Amer Mahmood verfasserin aut In Journal of Water and Climate Change IWA Publishing, 2021 13(2022), 11, Seite 3977-3999 (DE-627)62604703X (DE-600)2552186-X 24089354 nnns volume:13 year:2022 number:11 pages:3977-3999 https://doi.org/10.2166/wcc.2022.261 kostenfrei https://doaj.org/article/5c3e9fcf300c425193d9478fa67425c1 kostenfrei http://jwcc.iwaponline.com/content/13/11/3977 kostenfrei https://doaj.org/toc/2040-2244 Journal toc kostenfrei https://doaj.org/toc/2408-9354 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_4046 AR 13 2022 11 3977-3999
allfields_unstemmed	10.2166/wcc.2022.261 doi (DE-627)DOAJ026400502 (DE-599)DOAJ5c3e9fcf300c425193d9478fa67425c1 DE-627 ger DE-627 rakwb eng TD1-1066 GE1-350 Jamal Hassan Ougahi verfasserin aut Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Hydrological models play a key role in simulating and assessing climate and land use/cover (LULC) change impacts on hydrology in a watershed. In this study, the impact of climate and LULC change was investigated using the Soil and Water Assessment Tool (SWAT) model. The simulated and observed streamflow showed a good agreement. Both Nash–Sutcliffe Efficiency (NSE) and coefficient of determination (R2) were found to be greater than 0.7 during the calibration (1985–2002) and validation (2003–2012) period. The water balance components were simulated with inputs from downscaled Global Climate Models (GCMs) data (i.e., future scenario (2030–2100) relative to a baseline period (1974–2004)) under RCP4.5 and RCP8.5, and hypothetical generated LULC change scenarios. All GCMs projected an increase in temperature over the Kabul River Basin (KRB), whereas there was a lack of agreement on projected precipitation among GCMs under both emission and future scenarios. Water yield (WYLD) and evapotranspiration (ET) were projected to decrease in the 21st century. Average annual WYLD was projected to increase under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios. These results are valuable for relevant agencies and stakeholders to adopt measures to counter the negative impacts of climate and LULC change on water resources. HIGHLIGHTS The projected temperature consistently increases in the 21st century.; Most of the GCMs projected a decrease in annual and winter precipitation in the KRB.; The simulated water balance components show a higher impact by climate than LULC change scenarios.; The water yield was increased under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios.; climate change kabul river basin land use change swat model water balance components Environmental technology. Sanitary engineering Environmental sciences Shahid Karim verfasserin aut Syed Amer Mahmood verfasserin aut In Journal of Water and Climate Change IWA Publishing, 2021 13(2022), 11, Seite 3977-3999 (DE-627)62604703X (DE-600)2552186-X 24089354 nnns volume:13 year:2022 number:11 pages:3977-3999 https://doi.org/10.2166/wcc.2022.261 kostenfrei https://doaj.org/article/5c3e9fcf300c425193d9478fa67425c1 kostenfrei http://jwcc.iwaponline.com/content/13/11/3977 kostenfrei https://doaj.org/toc/2040-2244 Journal toc kostenfrei https://doaj.org/toc/2408-9354 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_4046 AR 13 2022 11 3977-3999
allfieldsGer	10.2166/wcc.2022.261 doi (DE-627)DOAJ026400502 (DE-599)DOAJ5c3e9fcf300c425193d9478fa67425c1 DE-627 ger DE-627 rakwb eng TD1-1066 GE1-350 Jamal Hassan Ougahi verfasserin aut Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Hydrological models play a key role in simulating and assessing climate and land use/cover (LULC) change impacts on hydrology in a watershed. In this study, the impact of climate and LULC change was investigated using the Soil and Water Assessment Tool (SWAT) model. The simulated and observed streamflow showed a good agreement. Both Nash–Sutcliffe Efficiency (NSE) and coefficient of determination (R2) were found to be greater than 0.7 during the calibration (1985–2002) and validation (2003–2012) period. The water balance components were simulated with inputs from downscaled Global Climate Models (GCMs) data (i.e., future scenario (2030–2100) relative to a baseline period (1974–2004)) under RCP4.5 and RCP8.5, and hypothetical generated LULC change scenarios. All GCMs projected an increase in temperature over the Kabul River Basin (KRB), whereas there was a lack of agreement on projected precipitation among GCMs under both emission and future scenarios. Water yield (WYLD) and evapotranspiration (ET) were projected to decrease in the 21st century. Average annual WYLD was projected to increase under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios. These results are valuable for relevant agencies and stakeholders to adopt measures to counter the negative impacts of climate and LULC change on water resources. HIGHLIGHTS The projected temperature consistently increases in the 21st century.; Most of the GCMs projected a decrease in annual and winter precipitation in the KRB.; The simulated water balance components show a higher impact by climate than LULC change scenarios.; The water yield was increased under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios.; climate change kabul river basin land use change swat model water balance components Environmental technology. Sanitary engineering Environmental sciences Shahid Karim verfasserin aut Syed Amer Mahmood verfasserin aut In Journal of Water and Climate Change IWA Publishing, 2021 13(2022), 11, Seite 3977-3999 (DE-627)62604703X (DE-600)2552186-X 24089354 nnns volume:13 year:2022 number:11 pages:3977-3999 https://doi.org/10.2166/wcc.2022.261 kostenfrei https://doaj.org/article/5c3e9fcf300c425193d9478fa67425c1 kostenfrei http://jwcc.iwaponline.com/content/13/11/3977 kostenfrei https://doaj.org/toc/2040-2244 Journal toc kostenfrei https://doaj.org/toc/2408-9354 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_4046 AR 13 2022 11 3977-3999
allfieldsSound	10.2166/wcc.2022.261 doi (DE-627)DOAJ026400502 (DE-599)DOAJ5c3e9fcf300c425193d9478fa67425c1 DE-627 ger DE-627 rakwb eng TD1-1066 GE1-350 Jamal Hassan Ougahi verfasserin aut Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Hydrological models play a key role in simulating and assessing climate and land use/cover (LULC) change impacts on hydrology in a watershed. In this study, the impact of climate and LULC change was investigated using the Soil and Water Assessment Tool (SWAT) model. The simulated and observed streamflow showed a good agreement. Both Nash–Sutcliffe Efficiency (NSE) and coefficient of determination (R2) were found to be greater than 0.7 during the calibration (1985–2002) and validation (2003–2012) period. The water balance components were simulated with inputs from downscaled Global Climate Models (GCMs) data (i.e., future scenario (2030–2100) relative to a baseline period (1974–2004)) under RCP4.5 and RCP8.5, and hypothetical generated LULC change scenarios. All GCMs projected an increase in temperature over the Kabul River Basin (KRB), whereas there was a lack of agreement on projected precipitation among GCMs under both emission and future scenarios. Water yield (WYLD) and evapotranspiration (ET) were projected to decrease in the 21st century. Average annual WYLD was projected to increase under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios. These results are valuable for relevant agencies and stakeholders to adopt measures to counter the negative impacts of climate and LULC change on water resources. HIGHLIGHTS The projected temperature consistently increases in the 21st century.; Most of the GCMs projected a decrease in annual and winter precipitation in the KRB.; The simulated water balance components show a higher impact by climate than LULC change scenarios.; The water yield was increased under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios.; climate change kabul river basin land use change swat model water balance components Environmental technology. Sanitary engineering Environmental sciences Shahid Karim verfasserin aut Syed Amer Mahmood verfasserin aut In Journal of Water and Climate Change IWA Publishing, 2021 13(2022), 11, Seite 3977-3999 (DE-627)62604703X (DE-600)2552186-X 24089354 nnns volume:13 year:2022 number:11 pages:3977-3999 https://doi.org/10.2166/wcc.2022.261 kostenfrei https://doaj.org/article/5c3e9fcf300c425193d9478fa67425c1 kostenfrei http://jwcc.iwaponline.com/content/13/11/3977 kostenfrei https://doaj.org/toc/2040-2244 Journal toc kostenfrei https://doaj.org/toc/2408-9354 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_4046 AR 13 2022 11 3977-3999
language	English
source	In Journal of Water and Climate Change 13(2022), 11, Seite 3977-3999 volume:13 year:2022 number:11 pages:3977-3999
sourceStr	In Journal of Water and Climate Change 13(2022), 11, Seite 3977-3999 volume:13 year:2022 number:11 pages:3977-3999
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	climate change kabul river basin land use change swat model water balance components Environmental technology. Sanitary engineering Environmental sciences
isfreeaccess_bool	true
container_title	Journal of Water and Climate Change
authorswithroles_txt_mv	Jamal Hassan Ougahi @@aut@@ Shahid Karim @@aut@@ Syed Amer Mahmood @@aut@@
publishDateDaySort_date	2022-01-01T00:00:00Z
hierarchy_top_id	62604703X
id	DOAJ026400502
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">DOAJ026400502</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230307101356.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230226s2022 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.2166/wcc.2022.261</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ026400502</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJ5c3e9fcf300c425193d9478fa67425c1</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="050" ind1=" " ind2="0"><subfield code="a">TD1-1066</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">GE1-350</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Jamal Hassan Ougahi</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</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">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Hydrological models play a key role in simulating and assessing climate and land use/cover (LULC) change impacts on hydrology in a watershed. In this study, the impact of climate and LULC change was investigated using the Soil and Water Assessment Tool (SWAT) model. The simulated and observed streamflow showed a good agreement. Both Nash–Sutcliffe Efficiency (NSE) and coefficient of determination (R2) were found to be greater than 0.7 during the calibration (1985–2002) and validation (2003–2012) period. The water balance components were simulated with inputs from downscaled Global Climate Models (GCMs) data (i.e., future scenario (2030–2100) relative to a baseline period (1974–2004)) under RCP4.5 and RCP8.5, and hypothetical generated LULC change scenarios. All GCMs projected an increase in temperature over the Kabul River Basin (KRB), whereas there was a lack of agreement on projected precipitation among GCMs under both emission and future scenarios. Water yield (WYLD) and evapotranspiration (ET) were projected to decrease in the 21st century. Average annual WYLD was projected to increase under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios. These results are valuable for relevant agencies and stakeholders to adopt measures to counter the negative impacts of climate and LULC change on water resources. HIGHLIGHTS The projected temperature consistently increases in the 21st century.; Most of the GCMs projected a decrease in annual and winter precipitation in the KRB.; The simulated water balance components show a higher impact by climate than LULC change scenarios.; The water yield was increased under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios.;</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">climate change</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">kabul river basin</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">land use change</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">swat model</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">water balance components</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Environmental technology. Sanitary engineering</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Environmental sciences</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Shahid Karim</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Syed Amer Mahmood</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Journal of Water and Climate Change</subfield><subfield code="d">IWA Publishing, 2021</subfield><subfield code="g">13(2022), 11, Seite 3977-3999</subfield><subfield code="w">(DE-627)62604703X</subfield><subfield code="w">(DE-600)2552186-X</subfield><subfield code="x">24089354</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:13</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:11</subfield><subfield code="g">pages:3977-3999</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.2166/wcc.2022.261</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/5c3e9fcf300c425193d9478fa67425c1</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://jwcc.iwaponline.com/content/13/11/3977</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2040-2244</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2408-9354</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</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_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</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_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4046</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">13</subfield><subfield code="j">2022</subfield><subfield code="e">11</subfield><subfield code="h">3977-3999</subfield></datafield></record></collection>
callnumber-first	T - Technology
author	Jamal Hassan Ougahi
spellingShingle	Jamal Hassan Ougahi misc TD1-1066 misc GE1-350 misc climate change misc kabul river basin misc land use change misc swat model misc water balance components misc Environmental technology. Sanitary engineering misc Environmental sciences Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan
authorStr	Jamal Hassan Ougahi
ppnlink_with_tag_str_mv	@@773@@(DE-627)62604703X
format	electronic Article
delete_txt_mv	keep
author_role	aut aut aut
collection	DOAJ
remote_str	true
callnumber-label	TD1-1066
illustrated	Not Illustrated
issn	24089354
topic_title	TD1-1066 GE1-350 Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan climate change kabul river basin land use change swat model water balance components
topic	misc TD1-1066 misc GE1-350 misc climate change misc kabul river basin misc land use change misc swat model misc water balance components misc Environmental technology. Sanitary engineering misc Environmental sciences
topic_unstemmed	misc TD1-1066 misc GE1-350 misc climate change misc kabul river basin misc land use change misc swat model misc water balance components misc Environmental technology. Sanitary engineering misc Environmental sciences
topic_browse	misc TD1-1066 misc GE1-350 misc climate change misc kabul river basin misc land use change misc swat model misc water balance components misc Environmental technology. Sanitary engineering misc Environmental sciences
format_facet	Elektronische Aufsätze Aufsätze Elektronische Ressource
format_main_str_mv	Text Zeitschrift/Artikel
carriertype_str_mv	cr
hierarchy_parent_title	Journal of Water and Climate Change
hierarchy_parent_id	62604703X
hierarchy_top_title	Journal of Water and Climate Change
isfreeaccess_txt	true
familylinks_str_mv	(DE-627)62604703X (DE-600)2552186-X
title	Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan
ctrlnum	(DE-627)DOAJ026400502 (DE-599)DOAJ5c3e9fcf300c425193d9478fa67425c1
title_full	Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan
author_sort	Jamal Hassan Ougahi
journal	Journal of Water and Climate Change
journalStr	Journal of Water and Climate Change
callnumber-first-code	T
lang_code	eng
isOA_bool	true
recordtype	marc
publishDateSort	2022
contenttype_str_mv	txt
container_start_page	3977
author_browse	Jamal Hassan Ougahi Shahid Karim Syed Amer Mahmood
container_volume	13
class	TD1-1066 GE1-350
format_se	Elektronische Aufsätze
author-letter	Jamal Hassan Ougahi
doi_str_mv	10.2166/wcc.2022.261
author2-role	verfasserin
title_sort	application of the swat model to assess climate and land use/cover change impacts on water balance components of the kabul river basin, afghanistan
callnumber	TD1-1066
title_auth	Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan
abstract	Hydrological models play a key role in simulating and assessing climate and land use/cover (LULC) change impacts on hydrology in a watershed. In this study, the impact of climate and LULC change was investigated using the Soil and Water Assessment Tool (SWAT) model. The simulated and observed streamflow showed a good agreement. Both Nash–Sutcliffe Efficiency (NSE) and coefficient of determination (R2) were found to be greater than 0.7 during the calibration (1985–2002) and validation (2003–2012) period. The water balance components were simulated with inputs from downscaled Global Climate Models (GCMs) data (i.e., future scenario (2030–2100) relative to a baseline period (1974–2004)) under RCP4.5 and RCP8.5, and hypothetical generated LULC change scenarios. All GCMs projected an increase in temperature over the Kabul River Basin (KRB), whereas there was a lack of agreement on projected precipitation among GCMs under both emission and future scenarios. Water yield (WYLD) and evapotranspiration (ET) were projected to decrease in the 21st century. Average annual WYLD was projected to increase under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios. These results are valuable for relevant agencies and stakeholders to adopt measures to counter the negative impacts of climate and LULC change on water resources. HIGHLIGHTS The projected temperature consistently increases in the 21st century.; Most of the GCMs projected a decrease in annual and winter precipitation in the KRB.; The simulated water balance components show a higher impact by climate than LULC change scenarios.; The water yield was increased under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios.;
abstractGer	Hydrological models play a key role in simulating and assessing climate and land use/cover (LULC) change impacts on hydrology in a watershed. In this study, the impact of climate and LULC change was investigated using the Soil and Water Assessment Tool (SWAT) model. The simulated and observed streamflow showed a good agreement. Both Nash–Sutcliffe Efficiency (NSE) and coefficient of determination (R2) were found to be greater than 0.7 during the calibration (1985–2002) and validation (2003–2012) period. The water balance components were simulated with inputs from downscaled Global Climate Models (GCMs) data (i.e., future scenario (2030–2100) relative to a baseline period (1974–2004)) under RCP4.5 and RCP8.5, and hypothetical generated LULC change scenarios. All GCMs projected an increase in temperature over the Kabul River Basin (KRB), whereas there was a lack of agreement on projected precipitation among GCMs under both emission and future scenarios. Water yield (WYLD) and evapotranspiration (ET) were projected to decrease in the 21st century. Average annual WYLD was projected to increase under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios. These results are valuable for relevant agencies and stakeholders to adopt measures to counter the negative impacts of climate and LULC change on water resources. HIGHLIGHTS The projected temperature consistently increases in the 21st century.; Most of the GCMs projected a decrease in annual and winter precipitation in the KRB.; The simulated water balance components show a higher impact by climate than LULC change scenarios.; The water yield was increased under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios.;
abstract_unstemmed	Hydrological models play a key role in simulating and assessing climate and land use/cover (LULC) change impacts on hydrology in a watershed. In this study, the impact of climate and LULC change was investigated using the Soil and Water Assessment Tool (SWAT) model. The simulated and observed streamflow showed a good agreement. Both Nash–Sutcliffe Efficiency (NSE) and coefficient of determination (R2) were found to be greater than 0.7 during the calibration (1985–2002) and validation (2003–2012) period. The water balance components were simulated with inputs from downscaled Global Climate Models (GCMs) data (i.e., future scenario (2030–2100) relative to a baseline period (1974–2004)) under RCP4.5 and RCP8.5, and hypothetical generated LULC change scenarios. All GCMs projected an increase in temperature over the Kabul River Basin (KRB), whereas there was a lack of agreement on projected precipitation among GCMs under both emission and future scenarios. Water yield (WYLD) and evapotranspiration (ET) were projected to decrease in the 21st century. Average annual WYLD was projected to increase under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios. These results are valuable for relevant agencies and stakeholders to adopt measures to counter the negative impacts of climate and LULC change on water resources. HIGHLIGHTS The projected temperature consistently increases in the 21st century.; Most of the GCMs projected a decrease in annual and winter precipitation in the KRB.; The simulated water balance components show a higher impact by climate than LULC change scenarios.; The water yield was increased under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios.;
collection_details	GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_4046
container_issue	11
title_short	Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan
url	https://doi.org/10.2166/wcc.2022.261 https://doaj.org/article/5c3e9fcf300c425193d9478fa67425c1 http://jwcc.iwaponline.com/content/13/11/3977 https://doaj.org/toc/2040-2244 https://doaj.org/toc/2408-9354
remote_bool	true
author2	Shahid Karim Syed Amer Mahmood
author2Str	Shahid Karim Syed Amer Mahmood
ppnlink	62604703X
callnumber-subject	TD - Environmental Technology
mediatype_str_mv	c
isOA_txt	true
hochschulschrift_bool	false
doi_str	10.2166/wcc.2022.261
callnumber-a	TD1-1066
up_date	2024-07-03T20:46:13.910Z
_version_	1803592216256446464
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">DOAJ026400502</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230307101356.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230226s2022 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.2166/wcc.2022.261</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ026400502</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJ5c3e9fcf300c425193d9478fa67425c1</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="050" ind1=" " ind2="0"><subfield code="a">TD1-1066</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">GE1-350</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Jamal Hassan Ougahi</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</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">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Hydrological models play a key role in simulating and assessing climate and land use/cover (LULC) change impacts on hydrology in a watershed. In this study, the impact of climate and LULC change was investigated using the Soil and Water Assessment Tool (SWAT) model. The simulated and observed streamflow showed a good agreement. Both Nash–Sutcliffe Efficiency (NSE) and coefficient of determination (R2) were found to be greater than 0.7 during the calibration (1985–2002) and validation (2003–2012) period. The water balance components were simulated with inputs from downscaled Global Climate Models (GCMs) data (i.e., future scenario (2030–2100) relative to a baseline period (1974–2004)) under RCP4.5 and RCP8.5, and hypothetical generated LULC change scenarios. All GCMs projected an increase in temperature over the Kabul River Basin (KRB), whereas there was a lack of agreement on projected precipitation among GCMs under both emission and future scenarios. Water yield (WYLD) and evapotranspiration (ET) were projected to decrease in the 21st century. Average annual WYLD was projected to increase under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios. These results are valuable for relevant agencies and stakeholders to adopt measures to counter the negative impacts of climate and LULC change on water resources. HIGHLIGHTS The projected temperature consistently increases in the 21st century.; Most of the GCMs projected a decrease in annual and winter precipitation in the KRB.; The simulated water balance components show a higher impact by climate than LULC change scenarios.; The water yield was increased under the agriculture-dominant scenario, whereas it decreased under forest and grassland-dominant scenarios.;</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">climate change</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">kabul river basin</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">land use change</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">swat model</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">water balance components</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Environmental technology. Sanitary engineering</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Environmental sciences</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Shahid Karim</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Syed Amer Mahmood</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Journal of Water and Climate Change</subfield><subfield code="d">IWA Publishing, 2021</subfield><subfield code="g">13(2022), 11, Seite 3977-3999</subfield><subfield code="w">(DE-627)62604703X</subfield><subfield code="w">(DE-600)2552186-X</subfield><subfield code="x">24089354</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:13</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:11</subfield><subfield code="g">pages:3977-3999</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.2166/wcc.2022.261</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/5c3e9fcf300c425193d9478fa67425c1</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://jwcc.iwaponline.com/content/13/11/3977</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2040-2244</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2408-9354</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</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_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</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_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4046</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">13</subfield><subfield code="j">2022</subfield><subfield code="e">11</subfield><subfield code="h">3977-3999</subfield></datafield></record></collection>
score	7.4028063

Nicht das Richtige dabei?

Schreiben Sie uns!

Application of the SWAT model to assess climate and land use/cover change impacts on water balance components of the Kabul River Basin, Afghanistan

Nicht das Richtige dabei?

Zugang & Verfügbarkeit

Vorhandene Bände

Nicht das Richtige dabei?