FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4383819172> ?p ?o ?g. }

• W4383819172 endingPage "3460" @default.
• W4383819172 startingPage "3460" @default.
• W4383819172 abstract "A large number of different-sized lakes exist in the inland area of the Tibetan Plateau (TP), which are examples of the important connection between the atmosphere and hydrosphere through the analysis of lake surface convergence and evaporation processes. The evaporation level changes that occur in middle–large-sized lakes (surface area > 50 km2) in the area directly influence the regional mass and energy balance values, atmospheric boundary layer heat and humidity structures, and weather processes occurring in the lower-reach areas. The studies conducted in the literature at present, concerning lake evaporation processes, generally overlook the differences in lake heat storage behavior due to the reduced amount of data in the literature concerning lake bathymetry. According to the in situ bathymetric data obtained for 68 middle–large-sized lakes in the inner basin of the TP, in this study, we calculated their heat storage (G) change values by using the different vertical-depth water-temperature-change integral method, and we established a regression equation for the heat storage and lake surface net radiation values for 68 lakes. The evaporation rates of 134 middle–large-sized lakes larger than 50 km2 in the inland are of the TP were calculated by obtaining the G regression result and adopting it into the Penman model, as well as estimating the evaporation losses of theses 134 lakes from 2002 to 2018. The result shows that the annual average evaporation rate for these lakes is 927.39 mm/year, with an insignificant upward trend (0.10 mm/year). This method achieved good accuracy compared with the Bowen ratio method, which estimates the evaporation rate during the ice-free season, with a high correlation coefficient (R) value of 0.95 and least root mean square error (RMSE) value of 61 mm. The annual mean evaporation rate can be divided into the southern and northern lake groups along a 34°N line with a difference of 314.41 mm/year. The annual average evaporation volume of these lakes was 25.02 km3 and showed an upward trend of 0.35 km3/year. Among them, the annual average evaporation volume contribution ratio of level-1 lakes (50 km2 ≤ lake’s area < 100 km2, 61 lakes) was 14.04%, showing an upward trend, and the contribution of level-3 lakes (lake’s area ≥ 500 km2, 10 lakes) was 41.50%, showing a downward trend. There were no obvious changes in the level-2 lakes (100 km2 ≤ lake’s area < 500 km2, 63 lakes), which maintained at the same level in approximately 44.46%. Air temperature is the most important factor affecting the evaporation rate of lakes, while the lake surface area is the main factor affecting lake evaporation volume. Our study, considering the actual lake heat storage value, provides a useful reference for further improving lake water budget balance values and watershed hydrologic features in the inland closed lakes located in the TP." @default.
• W4383819172 created "2023-07-11" @default.
• W4383819172 creator A5014102455 @default.
• W4383819172 creator A5021131841 @default.
• W4383819172 creator A5034084187 @default.
• W4383819172 creator A5051202580 @default.
• W4383819172 creator A5056914586 @default.
• W4383819172 creator A5073721879 @default.
• W4383819172 date "2023-07-08" @default.
• W4383819172 modified "2023-10-05" @default.
• W4383819172 title "A Quantification of Heat Storage Change-Based Evaporation Behavior in Middle–Large-Sized Lakes in the Inland of the Tibetan Plateau and Their Temporal and Spatial Variations" @default.
• W4383819172 cites W1143095904 @default.
• W4383819172 cites W1629256440 @default.
• W4383819172 cites W1882187602 @default.
• W4383819172 cites W1968350714 @default.
• W4383819172 cites W1971065291 @default.
• W4383819172 cites W1976984800 @default.
• W4383819172 cites W1997323379 @default.
• W4383819172 cites W2014685194 @default.
• W4383819172 cites W2024583496 @default.
• W4383819172 cites W2046431283 @default.
• W4383819172 cites W2056356839 @default.
• W4383819172 cites W2065259248 @default.
• W4383819172 cites W2076732124 @default.
• W4383819172 cites W2082934097 @default.
• W4383819172 cites W2136173208 @default.
• W4383819172 cites W2143077373 @default.
• W4383819172 cites W2265369130 @default.
• W4383819172 cites W2270792293 @default.
• W4383819172 cites W2305233962 @default.
• W4383819172 cites W2366982674 @default.
• W4383819172 cites W2461785475 @default.
• W4383819172 cites W2507506815 @default.
• W4383819172 cites W2560167313 @default.
• W4383819172 cites W2570221118 @default.
• W4383819172 cites W2611057588 @default.
• W4383819172 cites W2743841931 @default.
• W4383819172 cites W2777575601 @default.
• W4383819172 cites W2808624207 @default.
• W4383819172 cites W2808903917 @default.
• W4383819172 cites W2908939395 @default.
• W4383819172 cites W2914331787 @default.
• W4383819172 cites W2915537200 @default.
• W4383819172 cites W2929999089 @default.
• W4383819172 cites W2935378140 @default.
• W4383819172 cites W2938086739 @default.
• W4383819172 cites W2961182574 @default.
• W4383819172 cites W2962702674 @default.
• W4383819172 cites W2969709240 @default.
• W4383819172 cites W2988353138 @default.
• W4383819172 cites W2989933183 @default.
• W4383819172 cites W2991329086 @default.
• W4383819172 cites W2992820108 @default.
• W4383819172 cites W3002343708 @default.
• W4383819172 cites W3037463020 @default.
• W4383819172 cites W3040818127 @default.
• W4383819172 cites W3046590992 @default.
• W4383819172 cites W3079641317 @default.
• W4383819172 cites W3087451357 @default.
• W4383819172 cites W3088384284 @default.
• W4383819172 cites W3118879673 @default.
• W4383819172 cites W3133072772 @default.
• W4383819172 cites W3133744864 @default.
• W4383819172 cites W3134096290 @default.
• W4383819172 cites W3169870901 @default.
• W4383819172 cites W3180171032 @default.
• W4383819172 cites W3188977224 @default.
• W4383819172 cites W3204213683 @default.
• W4383819172 cites W4281693171 @default.
• W4383819172 doi "https://doi.org/10.3390/rs15143460" @default.
• W4383819172 hasPublicationYear "2023" @default.
• W4383819172 type Work @default.
• W4383819172 citedByCount "1" @default.
• W4383819172 countsByYear W43838191722023 @default.
• W4383819172 crossrefType "journal-article" @default.
• W4383819172 hasAuthorship W4383819172A5014102455 @default.
• W4383819172 hasAuthorship W4383819172A5021131841 @default.
• W4383819172 hasAuthorship W4383819172A5034084187 @default.
• W4383819172 hasAuthorship W4383819172A5051202580 @default.
• W4383819172 hasAuthorship W4383819172A5056914586 @default.
• W4383819172 hasAuthorship W4383819172A5073721879 @default.
• W4383819172 hasBestOaLocation W43838191721 @default.
• W4383819172 hasConcept C107218244 @default.
• W4383819172 hasConcept C109007969 @default.
• W4383819172 hasConcept C111368507 @default.
• W4383819172 hasConcept C114793014 @default.
• W4383819172 hasConcept C126026641 @default.
• W4383819172 hasConcept C127313418 @default.
• W4383819172 hasConcept C134306372 @default.
• W4383819172 hasConcept C151420433 @default.
• W4383819172 hasConcept C153294291 @default.
• W4383819172 hasConcept C158960510 @default.
• W4383819172 hasConcept C174943157 @default.
• W4383819172 hasConcept C187320778 @default.
• W4383819172 hasConcept C18903297 @default.
• W4383819172 hasConcept C205649164 @default.
• W4383819172 hasConcept C23430798 @default.
• W4383819172 hasConcept C2780030769 @default.

• next