FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4313281837> ?p ?o ?g. }

• W4313281837 endingPage "6350" @default.
• W4313281837 startingPage "6350" @default.
• W4313281837 abstract "The monitoring of permafrost is important for assessing the effects of global environmental changes and maintaining and managing social infrastructure, and remote sensing is increasingly being used for this wide-area monitoring. However, the accuracy of the conventional method in terms of temperature factor and soil factor needs to be improved. To address these two issues, in this study, we propose a new model to evaluate permafrost with a higher accuracy than the conventional methods. In this model, the land surface temperature (LST) is used as the upper temperature of the active layer of permafrost, and the temperature at the top of permafrost (TTOP) is used as the lower temperature. The TTOP value is then calculated by a modified equation using precipitation–evapotranspiration (PE) factors to account for the effect of soil moisture. This model, referred to as the TTOP-LST zero-curtain (TLZ) model, allows us to analyze subsurface temperatures for each layer of the active layer, and to evaluate the presence or absence of the zero-curtain effect through a time series analysis of stratified subsurface temperatures. The model was applied to the Qinghai–Tibetan Plateau and permafrost was classified into seven classes based on aspects such as stability and seasonality. As a result, it was possible to map the recent deterioration of permafrost in this region, which is thought to be caused by global warming. A comparison with the mean annual ground temperature (MAGT) model using local subsurface temperature data showed that the average root mean square error (RMSE) value of subsurface temperatures at different depths was 0.19 degrees C, indicating the validity of the TLZ model. A similar analysis based on the TLZ model is expected to enable detailed permafrost analysis in other areas." @default.
• W4313281837 created "2023-01-06" @default.
• W4313281837 creator A5051758340 @default.
• W4313281837 creator A5053184529 @default.
• W4313281837 date "2022-12-15" @default.
• W4313281837 modified "2023-10-18" @default.
• W4313281837 title "Analysis of Permafrost Distribution and Change in the Mid-East Qinghai–Tibetan Plateau during 2012–2021 Using the New TLZ Model" @default.
• W4313281837 cites W150302184 @default.
• W4313281837 cites W1526406783 @default.
• W4313281837 cites W1773127980 @default.
• W4313281837 cites W1966590364 @default.
• W4313281837 cites W1970423582 @default.
• W4313281837 cites W1970549237 @default.
• W4313281837 cites W1975014117 @default.
• W4313281837 cites W1980590347 @default.
• W4313281837 cites W1981028777 @default.
• W4313281837 cites W1981711737 @default.
• W4313281837 cites W1994296880 @default.
• W4313281837 cites W1995814302 @default.
• W4313281837 cites W2008480759 @default.
• W4313281837 cites W2011216226 @default.
• W4313281837 cites W2016094676 @default.
• W4313281837 cites W2021590014 @default.
• W4313281837 cites W2030342673 @default.
• W4313281837 cites W2032459157 @default.
• W4313281837 cites W2063073065 @default.
• W4313281837 cites W2072806535 @default.
• W4313281837 cites W2075794274 @default.
• W4313281837 cites W2076271908 @default.
• W4313281837 cites W2076321840 @default.
• W4313281837 cites W2082888108 @default.
• W4313281837 cites W2091515622 @default.
• W4313281837 cites W2094242026 @default.
• W4313281837 cites W2129594740 @default.
• W4313281837 cites W2132298983 @default.
• W4313281837 cites W2157645981 @default.
• W4313281837 cites W2159555251 @default.
• W4313281837 cites W2163819245 @default.
• W4313281837 cites W2425845278 @default.
• W4313281837 cites W2432405417 @default.
• W4313281837 cites W2534439660 @default.
• W4313281837 cites W2565203678 @default.
• W4313281837 cites W2605334580 @default.
• W4313281837 cites W2751261270 @default.
• W4313281837 cites W2765241381 @default.
• W4313281837 cites W2766039791 @default.
• W4313281837 cites W2766337505 @default.
• W4313281837 cites W2802034263 @default.
• W4313281837 cites W2899555154 @default.
• W4313281837 cites W2942435959 @default.
• W4313281837 cites W2967350082 @default.
• W4313281837 cites W2969677287 @default.
• W4313281837 cites W3001001561 @default.
• W4313281837 cites W3007068437 @default.
• W4313281837 cites W3008384792 @default.
• W4313281837 cites W3012806629 @default.
• W4313281837 cites W3024987409 @default.
• W4313281837 cites W3042934645 @default.
• W4313281837 cites W3044673747 @default.
• W4313281837 cites W3091622621 @default.
• W4313281837 cites W3122585005 @default.
• W4313281837 cites W3149821648 @default.
• W4313281837 cites W3158248111 @default.
• W4313281837 cites W3160618725 @default.
• W4313281837 cites W3197468152 @default.
• W4313281837 cites W3208260154 @default.
• W4313281837 cites W4220910026 @default.
• W4313281837 cites W4229050049 @default.
• W4313281837 cites W4251391067 @default.
• W4313281837 cites W4280589324 @default.
• W4313281837 cites W4281863136 @default.
• W4313281837 cites W4296194165 @default.
• W4313281837 cites W4361755727 @default.
• W4313281837 doi "https://doi.org/10.3390/rs14246350" @default.
• W4313281837 hasPublicationYear "2022" @default.
• W4313281837 type Work @default.
• W4313281837 citedByCount "0" @default.
• W4313281837 crossrefType "journal-article" @default.
• W4313281837 hasAuthorship W4313281837A5051758340 @default.
• W4313281837 hasAuthorship W4313281837A5053184529 @default.
• W4313281837 hasBestOaLocation W43132818371 @default.
• W4313281837 hasConcept C100970517 @default.
• W4313281837 hasConcept C107054158 @default.
• W4313281837 hasConcept C111368507 @default.
• W4313281837 hasConcept C115343472 @default.
• W4313281837 hasConcept C127313418 @default.
• W4313281837 hasConcept C132651083 @default.
• W4313281837 hasConcept C134306372 @default.
• W4313281837 hasConcept C15098985 @default.
• W4313281837 hasConcept C153294291 @default.
• W4313281837 hasConcept C176783924 @default.
• W4313281837 hasConcept C178790620 @default.
• W4313281837 hasConcept C185592680 @default.
• W4313281837 hasConcept C187320778 @default.
• W4313281837 hasConcept C18903297 @default.
• W4313281837 hasConcept C205649164 @default.
• W4313281837 hasConcept C2776026197 @default.
• W4313281837 hasConcept C2779227376 @default.

• next