FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3132886145> ?p ?o ?g. }

• W3132886145 endingPage "145895" @default.
• W3132886145 startingPage "145895" @default.
• W3132886145 abstract "In the Upper Indus Basin (UIB), precipitation associated with synoptic-scale circulations impinges on the complex and steep orography of the western Himalaya and Karakoram. Heavy rainfall often falls over the foothills, frequently triggering landslides there. This study explores the role of these synoptic-scale circulations – extratropical western disturbances (WDs) and tropical depressions (TDs) – in producing the conducive conditions necessary to trigger landslides, using data from the NASA Global Landslide Catalog and WD and TD track databases. During the winter (October to April), UIB landslides peak in February and occur at a rate of 0.05 day−1, 61% of which are associated with the passage of a WD. They are most common when a WD is located within a few hundred kilometres of 30°N, and significantly rarer if the WD is north of 40°N. WDs provide moist southwesterly flow from the Arabian Sea and Mediterranean Sea to the UIB, resulting in large-scale precipitation, but landslide probability is not related to WD intensity. Non-WD winter landslides are associated with small-scale orographic precipitation that we hypothesise is due to cloudbursts. During the summer (May to September), UIB landslides peak in August and occur at a rate of 0.11 day−1, 60% of which are associated with TD activity. Many of these TDs are found over central India, slightly south of the climatological monsoon trough, where they provide strong monsoonal southeasterlies to the UIB flowing along the Himalayas. Increased landslide frequency is also associated with TD activity over the southern Bay of Bengal (BoB), and it is hypothesised that this is related to monsoon break conditions. Landslide frequency is significantly correlated with TD intensity. Non-TD landslides are associated with a northwestward extension of the monsoon trough, providing southeasterly barrier flow to the UIB. Implications for forecasting and climate change are discussed." @default.
• W3132886145 created "2021-03-01" @default.
• W3132886145 creator A5021229235 @default.
• W3132886145 creator A5059966362 @default.
• W3132886145 date "2021-07-01" @default.
• W3132886145 modified "2023-09-27" @default.
• W3132886145 title "Synoptic-scale precursors of landslides in the western Himalaya and Karakoram" @default.
• W3132886145 cites W1821153150 @default.
• W3132886145 cites W1966272519 @default.
• W3132886145 cites W1994108694 @default.
• W3132886145 cites W2007462649 @default.
• W3132886145 cites W2009167816 @default.
• W3132886145 cites W2025646595 @default.
• W3132886145 cites W2030724367 @default.
• W3132886145 cites W2054477479 @default.
• W3132886145 cites W2054512946 @default.
• W3132886145 cites W2059516434 @default.
• W3132886145 cites W2061940746 @default.
• W3132886145 cites W2065219467 @default.
• W3132886145 cites W2073298425 @default.
• W3132886145 cites W2082784698 @default.
• W3132886145 cites W2091896272 @default.
• W3132886145 cites W2101140431 @default.
• W3132886145 cites W2121745948 @default.
• W3132886145 cites W2144377302 @default.
• W3132886145 cites W2144493162 @default.
• W3132886145 cites W2153656222 @default.
• W3132886145 cites W2157227910 @default.
• W3132886145 cites W2164980539 @default.
• W3132886145 cites W2172877736 @default.
• W3132886145 cites W2285509402 @default.
• W3132886145 cites W2290407957 @default.
• W3132886145 cites W2313288002 @default.
• W3132886145 cites W2595615092 @default.
• W3132886145 cites W2616483903 @default.
• W3132886145 cites W2766381676 @default.
• W3132886145 cites W2789512733 @default.
• W3132886145 cites W2792546905 @default.
• W3132886145 cites W2792958463 @default.
• W3132886145 cites W2807909371 @default.
• W3132886145 cites W2900100665 @default.
• W3132886145 cites W2912398867 @default.
• W3132886145 cites W2944844101 @default.
• W3132886145 cites W2953601665 @default.
• W3132886145 cites W2956036856 @default.
• W3132886145 cites W3006071021 @default.
• W3132886145 cites W3036509456 @default.
• W3132886145 cites W3210767993 @default.
• W3132886145 cites W4206137632 @default.
• W3132886145 doi "https://doi.org/10.1016/j.scitotenv.2021.145895" @default.
• W3132886145 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/33647669" @default.
• W3132886145 hasPublicationYear "2021" @default.
• W3132886145 type Work @default.
• W3132886145 sameAs 3132886145 @default.
• W3132886145 citedByCount "9" @default.
• W3132886145 countsByYear W31328861452021 @default.
• W3132886145 countsByYear W31328861452022 @default.
• W3132886145 countsByYear W31328861452023 @default.
• W3132886145 crossrefType "journal-article" @default.
• W3132886145 hasAuthorship W3132886145A5021229235 @default.
• W3132886145 hasAuthorship W3132886145A5059966362 @default.
• W3132886145 hasBestOaLocation W31328861452 @default.
• W3132886145 hasConcept C107054158 @default.
• W3132886145 hasConcept C109007969 @default.
• W3132886145 hasConcept C114793014 @default.
• W3132886145 hasConcept C127313418 @default.
• W3132886145 hasConcept C129536444 @default.
• W3132886145 hasConcept C134295995 @default.
• W3132886145 hasConcept C136996986 @default.
• W3132886145 hasConcept C153294291 @default.
• W3132886145 hasConcept C186295008 @default.
• W3132886145 hasConcept C194507410 @default.
• W3132886145 hasConcept C205649164 @default.
• W3132886145 hasConcept C49204034 @default.
• W3132886145 hasConcept C58640448 @default.
• W3132886145 hasConceptScore W3132886145C107054158 @default.
• W3132886145 hasConceptScore W3132886145C109007969 @default.
• W3132886145 hasConceptScore W3132886145C114793014 @default.
• W3132886145 hasConceptScore W3132886145C127313418 @default.
• W3132886145 hasConceptScore W3132886145C129536444 @default.
• W3132886145 hasConceptScore W3132886145C134295995 @default.
• W3132886145 hasConceptScore W3132886145C136996986 @default.
• W3132886145 hasConceptScore W3132886145C153294291 @default.
• W3132886145 hasConceptScore W3132886145C186295008 @default.
• W3132886145 hasConceptScore W3132886145C194507410 @default.
• W3132886145 hasConceptScore W3132886145C205649164 @default.
• W3132886145 hasConceptScore W3132886145C49204034 @default.
• W3132886145 hasConceptScore W3132886145C58640448 @default.
• W3132886145 hasFunder F4320312420 @default.
• W3132886145 hasLocation W31328861451 @default.
• W3132886145 hasLocation W31328861452 @default.
• W3132886145 hasOpenAccess W3132886145 @default.
• W3132886145 hasPrimaryLocation W31328861451 @default.
• W3132886145 hasRelatedWork W1958377557 @default.
• W3132886145 hasRelatedWork W2049885513 @default.
• W3132886145 hasRelatedWork W2111228609 @default.
• W3132886145 hasRelatedWork W2216018963 @default.
• W3132886145 hasRelatedWork W2584615698 @default.

• next