FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4319878488> ?p ?o ?g. }

• W4319878488 abstract "Due to climate warming and increased precipitation, the permafrost of the Tibet Plateau (TP) has undergone serious degradation along with obvious lake expansion in recent decades. Model simulation is often used to analyze the contribution of permafrost melting to lake expansion, which may have many limitations. Taking Hohxil Lake (HL) basin over north TP as an example, this study makes full use of Sentinel-1 images by an improved small baseline subset interferometric technique (SBAS-InSAR), monitors the permafrost deformation from 2015 to 2020, and estimates its contribution to the lake expansion. The results show that the permafrost settlements mainly occur in the flat terrain around HL. The average line of sight (LOS) de-formation rate of permafrost is -3.59 ± 0.001 cm/yr, where there existed many obvious funnel-shaped thawing areas around the lake, indicating a close relationship between lake expansion and permafrost under-ground ice melting. The long-term linear deformation rate of underground ice is inverted by the traditional linear model, and the melting rate is estimated to be (31.17 ± 0.0054) ×10⁶ m³/yr with 9.3% contribution to the HL expansion. This study takes full advantage of Interferometric Synthetic Aperture Radar (InSAR) to quantitatively analyze the contribution of permafrost to lake expansion, which provides a new insight into the study of permafrost hydrological process and the proposed method can be easily extended to analyze lake water budget for underground ice in other watershed over the TP." @default.
• W4319878488 created "2023-02-11" @default.
• W4319878488 creator A5010657578 @default.
• W4319878488 creator A5053209536 @default.
• W4319878488 creator A5056815618 @default.
• W4319878488 creator A5057808954 @default.
• W4319878488 creator A5073453307 @default.
• W4319878488 creator A5083246490 @default.
• W4319878488 creator A5085675242 @default.
• W4319878488 date "2023-02-10" @default.
• W4319878488 modified "2023-10-18" @default.
• W4319878488 title "Estimating contribution of permafrost to lake expansion by SBAS-InSAR: a case study from Hohxil Lake basin in the Tibetan Plateau" @default.
• W4319878488 cites W1664171571 @default.
• W4319878488 cites W1980118448 @default.
• W4319878488 cites W1984670836 @default.
• W4319878488 cites W1995646567 @default.
• W4319878488 cites W1997275345 @default.
• W4319878488 cites W2001278639 @default.
• W4319878488 cites W2016677955 @default.
• W4319878488 cites W2016903184 @default.
• W4319878488 cites W2026080049 @default.
• W4319878488 cites W2036671702 @default.
• W4319878488 cites W2041296175 @default.
• W4319878488 cites W2042020446 @default.
• W4319878488 cites W2084744129 @default.
• W4319878488 cites W2085585287 @default.
• W4319878488 cites W2117060272 @default.
• W4319878488 cites W2123632763 @default.
• W4319878488 cites W2131434734 @default.
• W4319878488 cites W2136173208 @default.
• W4319878488 cites W2152657318 @default.
• W4319878488 cites W2156606791 @default.
• W4319878488 cites W2169606039 @default.
• W4319878488 cites W2174009612 @default.
• W4319878488 cites W2174625957 @default.
• W4319878488 cites W2300704775 @default.
• W4319878488 cites W2322545094 @default.
• W4319878488 cites W2410135257 @default.
• W4319878488 cites W2460420635 @default.
• W4319878488 cites W2489750361 @default.
• W4319878488 cites W2516972307 @default.
• W4319878488 cites W2534439660 @default.
• W4319878488 cites W2534845115 @default.
• W4319878488 cites W2549856320 @default.
• W4319878488 cites W2743841931 @default.
• W4319878488 cites W2789987199 @default.
• W4319878488 cites W2796567926 @default.
• W4319878488 cites W2899555154 @default.
• W4319878488 cites W2911087767 @default.
• W4319878488 cites W2921183019 @default.
• W4319878488 cites W2943415823 @default.
• W4319878488 cites W2976715433 @default.
• W4319878488 cites W2994847485 @default.
• W4319878488 cites W3004780320 @default.
• W4319878488 cites W3008246657 @default.
• W4319878488 cites W3020983980 @default.
• W4319878488 cites W3033578389 @default.
• W4319878488 cites W3037076994 @default.
• W4319878488 cites W3046899448 @default.
• W4319878488 cites W3093804892 @default.
• W4319878488 cites W3097098296 @default.
• W4319878488 cites W3124166242 @default.
• W4319878488 cites W3129165402 @default.
• W4319878488 cites W3135195673 @default.
• W4319878488 cites W3164952402 @default.
• W4319878488 cites W3214981759 @default.
• W4319878488 cites W4210727842 @default.
• W4319878488 cites W4232190828 @default.
• W4319878488 cites W4232869717 @default.
• W4319878488 cites W4248577798 @default.
• W4319878488 cites W4249104701 @default.
• W4319878488 cites W4256616295 @default.
• W4319878488 doi "https://doi.org/10.1117/12.2667888" @default.
• W4319878488 hasPublicationYear "2023" @default.
• W4319878488 type Work @default.
• W4319878488 citedByCount "0" @default.
• W4319878488 crossrefType "proceedings-article" @default.
• W4319878488 hasAuthorship W4319878488A5010657578 @default.
• W4319878488 hasAuthorship W4319878488A5053209536 @default.
• W4319878488 hasAuthorship W4319878488A5056815618 @default.
• W4319878488 hasAuthorship W4319878488A5057808954 @default.
• W4319878488 hasAuthorship W4319878488A5073453307 @default.
• W4319878488 hasAuthorship W4319878488A5083246490 @default.
• W4319878488 hasAuthorship W4319878488A5085675242 @default.
• W4319878488 hasConcept C100970517 @default.
• W4319878488 hasConcept C111368507 @default.
• W4319878488 hasConcept C114793014 @default.
• W4319878488 hasConcept C127313418 @default.
• W4319878488 hasConcept C134306372 @default.
• W4319878488 hasConcept C15098985 @default.
• W4319878488 hasConcept C161840515 @default.
• W4319878488 hasConcept C187320778 @default.
• W4319878488 hasConcept C18903297 @default.
• W4319878488 hasConcept C205649164 @default.
• W4319878488 hasConcept C22286887 @default.
• W4319878488 hasConcept C2780030769 @default.
• W4319878488 hasConcept C33923547 @default.
• W4319878488 hasConcept C62649853 @default.
• W4319878488 hasConcept C76886044 @default.
• W4319878488 hasConcept C86803240 @default.

• next