Matches in SemOpenAlex for { <https://semopenalex.org/work/W3128701198> ?p ?o ?g. }
- W3128701198 endingPage "101206" @default.
- W3128701198 startingPage "101206" @default.
- W3128701198 abstract "• It is found that the large-scale temperature anomalies for the mid-Holocene (compared to the preindustrial) are significantly different in the low- and high-resolution versions • For boreal winter, differences are related to circulation changes caused by the response to thermal forcing in conjunction with orographic resolution. • For summer, shortwave cloud radiative forcing emerges as the predominant factor. • The simulated mid-Holocene temperature differences (low versus high resolution) reveals a response that regionally can exceed the anomalous mid-Holocene temperature anomaly. This study evaluates the dependence of simulated surface air temperatures on model resolution and orography for the mid-Holocene. Sensitivity experiments with the atmospheric general circulation model ECHAM5 are performed with low (∼3.75°, 19 vertical levels) and high (∼1.1°, 31 vertical levels) resolution. Results are compared to the respective preindustrial runs. It is found that the large-scale temperature anomalies for the mid-Holocene (compared to preindustrial) are significantly different in the low- and high-resolution versions. For boreal winter, differences are mainly related to circulation changes caused by the response to thermal forcing in conjunction with orographic resolution. For summer, shortwave cloud radiative forcing emerges as an important factor. The anomaly differences (low minus high resolution version) in the Northern Hemisphere are regionally as large as the anomalous mid-Holocene temperature signals. Furthermore, they depend on the applied surface boundary conditions. We conclude that the resolution matters for the Northern Hemisphere response in mid-Holocene simulations, which should be taken into account in model-model and data-model comparisons." @default.
- W3128701198 created "2021-02-15" @default.
- W3128701198 creator A5060737906 @default.
- W3128701198 creator A5065435352 @default.
- W3128701198 creator A5084874832 @default.
- W3128701198 date "2021-03-01" @default.
- W3128701198 modified "2023-09-24" @default.
- W3128701198 title "Resolution of the atmospheric model matters for the Northern Hemisphere Mid-Holocene climate" @default.
- W3128701198 cites W1015794860 @default.
- W3128701198 cites W1494716491 @default.
- W3128701198 cites W1912607455 @default.
- W3128701198 cites W1968176769 @default.
- W3128701198 cites W1982185059 @default.
- W3128701198 cites W1985015735 @default.
- W3128701198 cites W1988405148 @default.
- W3128701198 cites W1988592161 @default.
- W3128701198 cites W1991011332 @default.
- W3128701198 cites W1992037877 @default.
- W3128701198 cites W1992904499 @default.
- W3128701198 cites W1993171187 @default.
- W3128701198 cites W1993337472 @default.
- W3128701198 cites W1993452836 @default.
- W3128701198 cites W1995636511 @default.
- W3128701198 cites W1999759982 @default.
- W3128701198 cites W2000444336 @default.
- W3128701198 cites W2006865042 @default.
- W3128701198 cites W2010094196 @default.
- W3128701198 cites W2010896871 @default.
- W3128701198 cites W2011534840 @default.
- W3128701198 cites W2011725596 @default.
- W3128701198 cites W2012592445 @default.
- W3128701198 cites W2012978636 @default.
- W3128701198 cites W2015834247 @default.
- W3128701198 cites W2020733016 @default.
- W3128701198 cites W2020963742 @default.
- W3128701198 cites W2020978317 @default.
- W3128701198 cites W2021614821 @default.
- W3128701198 cites W2022834346 @default.
- W3128701198 cites W2024096099 @default.
- W3128701198 cites W2026925381 @default.
- W3128701198 cites W2029590672 @default.
- W3128701198 cites W2032658276 @default.
- W3128701198 cites W2034171120 @default.
- W3128701198 cites W2034387714 @default.
- W3128701198 cites W2034536992 @default.
- W3128701198 cites W2035587516 @default.
- W3128701198 cites W2035852128 @default.
- W3128701198 cites W2042290651 @default.
- W3128701198 cites W2045993787 @default.
- W3128701198 cites W2046753504 @default.
- W3128701198 cites W2050680642 @default.
- W3128701198 cites W2051387452 @default.
- W3128701198 cites W2055886783 @default.
- W3128701198 cites W2061154725 @default.
- W3128701198 cites W2061908320 @default.
- W3128701198 cites W2064444138 @default.
- W3128701198 cites W2065488127 @default.
- W3128701198 cites W2066691372 @default.
- W3128701198 cites W2067471069 @default.
- W3128701198 cites W2070399653 @default.
- W3128701198 cites W2071653738 @default.
- W3128701198 cites W2076848415 @default.
- W3128701198 cites W2080199880 @default.
- W3128701198 cites W2087624753 @default.
- W3128701198 cites W2088093247 @default.
- W3128701198 cites W2093479802 @default.
- W3128701198 cites W2099358694 @default.
- W3128701198 cites W2101000561 @default.
- W3128701198 cites W2101005049 @default.
- W3128701198 cites W2106405704 @default.
- W3128701198 cites W2112304371 @default.
- W3128701198 cites W2113323275 @default.
- W3128701198 cites W2113803029 @default.
- W3128701198 cites W2115957379 @default.
- W3128701198 cites W2117475318 @default.
- W3128701198 cites W2125600063 @default.
- W3128701198 cites W2126004720 @default.
- W3128701198 cites W2133101076 @default.
- W3128701198 cites W2139043127 @default.
- W3128701198 cites W2139199775 @default.
- W3128701198 cites W2140254733 @default.
- W3128701198 cites W2142644033 @default.
- W3128701198 cites W2143261564 @default.
- W3128701198 cites W2144026334 @default.
- W3128701198 cites W2151219339 @default.
- W3128701198 cites W2151920264 @default.
- W3128701198 cites W2157688053 @default.
- W3128701198 cites W2157698340 @default.
- W3128701198 cites W2160026318 @default.
- W3128701198 cites W2164268978 @default.
- W3128701198 cites W2176288461 @default.
- W3128701198 cites W2180215215 @default.
- W3128701198 cites W2180956791 @default.
- W3128701198 cites W2255021956 @default.
- W3128701198 cites W2289736227 @default.
- W3128701198 cites W2341047908 @default.
- W3128701198 cites W2517131503 @default.
- W3128701198 cites W2520629119 @default.