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dc.contributor.author김태웅-
dc.date.accessioned2024-04-16T02:28:59Z-
dc.date.available2024-04-16T02:28:59Z-
dc.date.issued2022-10-14-
dc.identifier.citationNATURAL HAZARDS, v. 115, NO 3, Page. 2483-2503en_US
dc.identifier.issn0921-030Xen_US
dc.identifier.issn1573-0840en_US
dc.identifier.urihttps://information.hanyang.ac.kr/#/eds/detail?an=edssjs.4767D0D1&dbId=edssjsen_US
dc.identifier.urihttps://repository.hanyang.ac.kr/handle/20.500.11754/189786-
dc.description.abstractClimate variation is a primary driving force influencing the hydrological cycle, resulting in extreme natural disasters such as drought. Investigating the linkage between meteorological and hydrological droughts under climate change is critical for early warning against hydrological drought. In this study, we investigated spatial and temporal characteristics of the drought propagation threshold (PT) in the Han River Basin (HRB) of South Korea. Standardized Precipitation Index (SPI) and Standardized Runoff Index (SRI) were employed to represent meteorological drought and hydrological drought, respectively. Correlation analyses between the SPI at various time scales (1-24 months) and the three-month SRI (SRI-3) were performed to identify the best time scale of SPI corresponding to the SRI-3. To investigate PTs, five general circulation models (GCMs) were selected to compute multi-model ensemble projections under Representative Concentration Pathway (RCP) 4.5 and 8.5 scenarios. A future period (2021-2099) was sub-divided into two periods such as P2 (2021-2060) and P3 (2061-2099) to estimate temporal variation of PT. Our results indicated that the SPI-4 showed the highest correlation with the SRI-3 in P1, while the SPI-3 best corresponded to the SRI-3 in future periods under both climate change scenarios. Drought characteristics of meteorological and hydrological drought showed increasing trends in P2 and P3 under both climate change scenarios. Spatio-temporal variation in PT was observed throughout the HRB. The PT showed significant decreases in both future periods, while the highest percentage decreases were observed in watersheds located in the northern, mid, and western parts of the HRB in P3 under both climate change scenarios.en_US
dc.languageen_USen_US
dc.publisherSPRINGERen_US
dc.relation.ispartofseriesv. 115, NO 3;2483-2503-
dc.subjectClimate changeen_US
dc.subjectDroughten_US
dc.subjectHan River Basinen_US
dc.subjectGCMsen_US
dc.subjectMulti-model ensembleen_US
dc.subjectNonlinear relationshipen_US
dc.subjectPropagation thresholden_US
dc.titleExploring spatio-temporal variation of drought characteristics and propagation under climate change using multi-model ensemble projectionsen_US
dc.typeArticleen_US
dc.relation.no3-
dc.relation.volume115-
dc.identifier.doi10.1007/s11069-022-05650-yen_US
dc.relation.page2483-2503-
dc.relation.journalNATURAL HAZARDS-
dc.contributor.googleauthorJehanzaib, Muhammad-
dc.contributor.googleauthorShah, Sabab Ali-
dc.contributor.googleauthorKim, Ji Eun-
dc.contributor.googleauthorKim, Tae-Woong-
dc.relation.code2023040401-
dc.sector.campusE-
dc.sector.daehakCOLLEGE OF ENGINEERING SCIENCES[E]-
dc.sector.departmentDEPARTMENT OF CIVIL AND ENVIRONMENTAL ENGINEERING-
dc.identifier.pidtwkim72-
Appears in Collections:
COLLEGE OF ENGINEERING SCIENCES[E](공학대학) > CIVIL AND ENVIRONMENTAL ENGINEERING(건설환경공학과) > Articles
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