Matches in SemOpenAlex for { <https://semopenalex.org/work/W4306673020> ?p ?o ?g. }
- W4306673020 endingPage "5194" @default.
- W4306673020 startingPage "5194" @default.
- W4306673020 abstract "Accurately monitoring spatio-temporal changes in lake water levels is important for studying the impacts of climate change on freshwater resources, and for predicting natural hazards. In this study, we applied multi-mission radar satellite altimetry data from the Laurentian Great Lakes, North America to optimally reconstruct multi-decadal lake-wide spatio-temporal changes of water level. We used the results to study physical processes such as teleconnections of El Niño and southern oscillation (ENSO) episodes over approximately the past three-and-a-half decades (1985–2018). First, we assessed three reconstruction methods, namely the standard empirical orthogonal function (EOF), complex EOF (CEOF), and complex independent component analysis (CICA), to model the lake-wide changes of water level. The performance of these techniques was evaluated using in-situ gauge data, after correcting the Glacial Isostatic Adjustment (GIA) process using a contemporary GIA forward model. While altimeter-measured water level was much less affected by GIA, the averaged gauge-measured water level was found to have increased up to 14 cm over the three decades. Our results indicate that the CICA-reconstructed 35-year lake level was more accurate than the other two techniques. The correlation coefficients between the CICA reconstruction and the in situ water-level data were 0.96, 0.99, 0.97, 0.97, and 0.95, for Lake Superior, Lake Michigan, Lake Huron, Lake Erie, and Lake Ontario, respectively; ~7% higher than the original altimetry data. The root mean squares of errors (RMSE) were 6.07 cm, 4.89 cm, 9.27 cm, 7.71 cm, and 9.88 cm, respectively, for each of the lakes, and ~44% less than differencing with the original altimetry data. Furthermore, the CICA results indicated that the water-level changes in the Great Lakes were significantly correlated with ENSO, with correlation coefficients of 0.5–0.8. The lake levels were ~25 cm higher (~30 cm lower) than normal during EI Niño (La Niña) events." @default.
- W4306673020 created "2022-10-19" @default.
- W4306673020 creator A5003554962 @default.
- W4306673020 creator A5016910459 @default.
- W4306673020 creator A5017335561 @default.
- W4306673020 creator A5017541508 @default.
- W4306673020 creator A5028070258 @default.
- W4306673020 creator A5031787313 @default.
- W4306673020 creator A5034026217 @default.
- W4306673020 creator A5035461057 @default.
- W4306673020 creator A5037185655 @default.
- W4306673020 creator A5037804613 @default.
- W4306673020 creator A5086828738 @default.
- W4306673020 date "2022-10-17" @default.
- W4306673020 modified "2023-09-27" @default.
- W4306673020 title "Understanding Water Level Changes in the Great Lakes by an ICA-Based Merging of Multi-Mission Altimetry Measurements" @default.
- W4306673020 cites W1516916808 @default.
- W4306673020 cites W1562504550 @default.
- W4306673020 cites W1590683087 @default.
- W4306673020 cites W1940180045 @default.
- W4306673020 cites W1979825716 @default.
- W4306673020 cites W1981147339 @default.
- W4306673020 cites W1983821361 @default.
- W4306673020 cites W1992521040 @default.
- W4306673020 cites W1993606461 @default.
- W4306673020 cites W1998494929 @default.
- W4306673020 cites W2001869302 @default.
- W4306673020 cites W2011714341 @default.
- W4306673020 cites W2024523255 @default.
- W4306673020 cites W2033602192 @default.
- W4306673020 cites W2035956818 @default.
- W4306673020 cites W2036971125 @default.
- W4306673020 cites W2039070965 @default.
- W4306673020 cites W2043893894 @default.
- W4306673020 cites W2045956279 @default.
- W4306673020 cites W2046177159 @default.
- W4306673020 cites W2048753484 @default.
- W4306673020 cites W2049448305 @default.
- W4306673020 cites W2053926920 @default.
- W4306673020 cites W2055176342 @default.
- W4306673020 cites W2061490253 @default.
- W4306673020 cites W2066114383 @default.
- W4306673020 cites W2069819970 @default.
- W4306673020 cites W2079390700 @default.
- W4306673020 cites W2086053994 @default.
- W4306673020 cites W2086886098 @default.
- W4306673020 cites W2087347023 @default.
- W4306673020 cites W2089472002 @default.
- W4306673020 cites W2091177453 @default.
- W4306673020 cites W2095110392 @default.
- W4306673020 cites W2103688971 @default.
- W4306673020 cites W2113453022 @default.
- W4306673020 cites W2123649031 @default.
- W4306673020 cites W2124757684 @default.
- W4306673020 cites W2144276939 @default.
- W4306673020 cites W2146129276 @default.
- W4306673020 cites W2150277639 @default.
- W4306673020 cites W2166361350 @default.
- W4306673020 cites W2174279521 @default.
- W4306673020 cites W2176233088 @default.
- W4306673020 cites W2178553074 @default.
- W4306673020 cites W2347066437 @default.
- W4306673020 cites W2778140962 @default.
- W4306673020 cites W2899601193 @default.
- W4306673020 cites W2921255895 @default.
- W4306673020 cites W3018260187 @default.
- W4306673020 cites W3145689897 @default.
- W4306673020 cites W4285807001 @default.
- W4306673020 doi "https://doi.org/10.3390/rs14205194" @default.
- W4306673020 hasPublicationYear "2022" @default.
- W4306673020 type Work @default.
- W4306673020 citedByCount "0" @default.
- W4306673020 crossrefType "journal-article" @default.
- W4306673020 hasAuthorship W4306673020A5003554962 @default.
- W4306673020 hasAuthorship W4306673020A5016910459 @default.
- W4306673020 hasAuthorship W4306673020A5017335561 @default.
- W4306673020 hasAuthorship W4306673020A5017541508 @default.
- W4306673020 hasAuthorship W4306673020A5028070258 @default.
- W4306673020 hasAuthorship W4306673020A5031787313 @default.
- W4306673020 hasAuthorship W4306673020A5034026217 @default.
- W4306673020 hasAuthorship W4306673020A5035461057 @default.
- W4306673020 hasAuthorship W4306673020A5037185655 @default.
- W4306673020 hasAuthorship W4306673020A5037804613 @default.
- W4306673020 hasAuthorship W4306673020A5086828738 @default.
- W4306673020 hasBestOaLocation W43066730201 @default.
- W4306673020 hasConcept C100970517 @default.
- W4306673020 hasConcept C111368507 @default.
- W4306673020 hasConcept C123576220 @default.
- W4306673020 hasConcept C127313418 @default.
- W4306673020 hasConcept C1284942 @default.
- W4306673020 hasConcept C132651083 @default.
- W4306673020 hasConcept C136856113 @default.
- W4306673020 hasConcept C13724139 @default.
- W4306673020 hasConcept C17534553 @default.
- W4306673020 hasConcept C187320778 @default.
- W4306673020 hasConcept C205649164 @default.
- W4306673020 hasConcept C39432304 @default.
- W4306673020 hasConcept C49204034 @default.