Matches in SemOpenAlex for { <https://semopenalex.org/work/W2372034648> ?p ?o ?g. }
Showing items 1 to 71 of
71
with 100 items per page.
- W2372034648 abstract "Plateau lakes are extremely sensitive to climate change, and climate change can be truly reflected through the variation of lakes. Based on multi-source and multi-date digital remote sensing images, topographic maps and digital elevation model(DEM) data, the lake boundaries were extracted with geographic information system and remote sensing technologies. Combined with other related research literatures, the area and boundary variation of Ulan Ul Lake in Hoh Xil Region and the correlation between such variations and the natural elements(annual mean temperature, annual precipitation, etc.) were analyzed from 1976 to 2012 in this study, and then the causes for such variations were also discussed through the angle of water balance of the lake. The results showed that Ulan Ul Lake had expanded on the whole during the period from 1976 to 2012, but experienced shrinkage first before the expansion. The lake was in a shrinkage during the period from 1976 to 1994 at a shrinkage rate of 3.12 km2/a, with its area varied from 555.97 km2in 1976 to 496.50 km2in 1994. A rapid expansion has started since 1998 with an expansion rate of 10.36 km2/a, and the lake area expanded from 499.83 km2in 1998 to 655.25 km2in 2012. In terms of space, the area variation of Ulan Ul Lake was mainly in the southern part where rives flow into the lake. The trends of meteorological factors over the Ulan Ul Lake basin from 1976 to 2012 showed the characteristics of increasing annual average temperature and increasing annual precipitation. There were a positive correlation between the annual mean temperature and the area of the lake. Comprehensive analysis revealed that the area variation of Ulan Ul Lake since 1998 was mainly caused by two factors, one was the increasing annual precipitation, and the other was the rising annual mean temperature, which leaded to the thawing of permafrost, ice and snow. Based on analysis of water balance of the lake, annual precipitation directly falling on lake, annual runoff deriving from the annual precipitation in the basin, and annual thawing water were the three main recharge resources of Ulan Ul Lake, respectively accounting for about 23.3%、43.7% and 33.0% of the total annual recharge quantity of the lake." @default.
- W2372034648 created "2016-06-24" @default.
- W2372034648 creator A5003111909 @default.
- W2372034648 date "2014-01-01" @default.
- W2372034648 modified "2023-09-26" @default.
- W2372034648 title "Variations of Lake Area and Boundary of Ulan Ul Lake in Hoh Xil Region during 1976-2012 and Their Reasons" @default.
- W2372034648 hasPublicationYear "2014" @default.
- W2372034648 type Work @default.
- W2372034648 sameAs 2372034648 @default.
- W2372034648 citedByCount "0" @default.
- W2372034648 crossrefType "journal-article" @default.
- W2372034648 hasAuthorship W2372034648A5003111909 @default.
- W2372034648 hasConcept C100970517 @default.
- W2372034648 hasConcept C107054158 @default.
- W2372034648 hasConcept C127313418 @default.
- W2372034648 hasConcept C132651083 @default.
- W2372034648 hasConcept C134306372 @default.
- W2372034648 hasConcept C153294291 @default.
- W2372034648 hasConcept C181843262 @default.
- W2372034648 hasConcept C187320778 @default.
- W2372034648 hasConcept C18903297 @default.
- W2372034648 hasConcept C205649164 @default.
- W2372034648 hasConcept C2780030769 @default.
- W2372034648 hasConcept C33923547 @default.
- W2372034648 hasConcept C39432304 @default.
- W2372034648 hasConcept C62649853 @default.
- W2372034648 hasConcept C76886044 @default.
- W2372034648 hasConcept C86803240 @default.
- W2372034648 hasConceptScore W2372034648C100970517 @default.
- W2372034648 hasConceptScore W2372034648C107054158 @default.
- W2372034648 hasConceptScore W2372034648C127313418 @default.
- W2372034648 hasConceptScore W2372034648C132651083 @default.
- W2372034648 hasConceptScore W2372034648C134306372 @default.
- W2372034648 hasConceptScore W2372034648C153294291 @default.
- W2372034648 hasConceptScore W2372034648C181843262 @default.
- W2372034648 hasConceptScore W2372034648C187320778 @default.
- W2372034648 hasConceptScore W2372034648C18903297 @default.
- W2372034648 hasConceptScore W2372034648C205649164 @default.
- W2372034648 hasConceptScore W2372034648C2780030769 @default.
- W2372034648 hasConceptScore W2372034648C33923547 @default.
- W2372034648 hasConceptScore W2372034648C39432304 @default.
- W2372034648 hasConceptScore W2372034648C62649853 @default.
- W2372034648 hasConceptScore W2372034648C76886044 @default.
- W2372034648 hasConceptScore W2372034648C86803240 @default.
- W2372034648 hasLocation W23720346481 @default.
- W2372034648 hasOpenAccess W2372034648 @default.
- W2372034648 hasPrimaryLocation W23720346481 @default.
- W2372034648 hasRelatedWork W1981068507 @default.
- W2372034648 hasRelatedWork W2000262703 @default.
- W2372034648 hasRelatedWork W2013301826 @default.
- W2372034648 hasRelatedWork W2035132379 @default.
- W2372034648 hasRelatedWork W2072232479 @default.
- W2372034648 hasRelatedWork W2130331356 @default.
- W2372034648 hasRelatedWork W2136173208 @default.
- W2372034648 hasRelatedWork W2158989104 @default.
- W2372034648 hasRelatedWork W2281699385 @default.
- W2372034648 hasRelatedWork W2348657824 @default.
- W2372034648 hasRelatedWork W2352515991 @default.
- W2372034648 hasRelatedWork W2376750657 @default.
- W2372034648 hasRelatedWork W2377180963 @default.
- W2372034648 hasRelatedWork W2388847076 @default.
- W2372034648 hasRelatedWork W2510107340 @default.
- W2372034648 hasRelatedWork W2588832182 @default.
- W2372034648 hasRelatedWork W2737635461 @default.
- W2372034648 hasRelatedWork W2767279551 @default.
- W2372034648 hasRelatedWork W2998802454 @default.
- W2372034648 hasRelatedWork W3027918029 @default.
- W2372034648 isParatext "false" @default.
- W2372034648 isRetracted "false" @default.
- W2372034648 magId "2372034648" @default.
- W2372034648 workType "article" @default.