FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2056520640> ?p ?o ?g. }

• W2056520640 abstract "[1] The horizontal spectrum of wind variance, conventionally referred to as the kinetic energy spectrum, is examined in experiments conducted with the Atmospheric GCM for the Earth Simulator (AFES) global spectral general circulation model. We find that the control version of AFES run at T639 horizontal spectral resolution simulates a kinetic energy spectrum that compares well at large scales with global observational reanalyses and, at smaller scales, with available aircraft observations at near-tropopause levels. Specifically there is a roughly −3 power-law dependence on horizontal wave number for wavelengths between about 5000 and 500 km, transitioning to a shallower mesoscale regime at smaller wavelengths. This is seen for both one-dimensional spectra and for the two-dimensional total wave number spectrum based on a spherical harmonic analysis. The simulated spectrum at midtropospheric levels is similar in that there is a transition to a shallower mesoscale regime, but the spectrum in the mesoscale is clearly steeper at midtroposphere than near the tropopause. There seem to be no extensive observations of horizontal spectra available in the midtroposphere, so it is not known whether the contrast seen in the model between upper and mid tropospheric levels is realistic. The dependence of the model simulated variability on the subgrid-scale moist convection parameterization is examined. The space-time variability of rainfall is shown to depend strongly on the convection scheme employed. The tropospheric kinetic energy spectrum in the mesoscale seems to be correlated with the precipitation behavior, so that in a version with a more variable precipitation field the kinetic energy in the mesoscale is enhanced. This suggests that the mesoscale motions in the model may be directly forced to a significant extent by the variability in the latent heating field. Experiments were also performed with a dry dynamical core version of the model run at both T639 and T1279 resolutions. This version also simulated a shallow mesoscale range, supporting the view that the mesoscale regime in the atmosphere is energized, at least in part, by a predominantly forward (i.e., downscale) nonlinear spectral cascade. Experiments with various formulations of the hyperdiffusion horizontal mixing parameterization show that the kinetic energy spectrum over about the last half of the resolved wave number range is under strong control by the parameterized mixing. However, the T1279 model simulates almost a decade of the shallow mesoscale regime (i.e., for horizontal wavelengths from about 80 to 500 km) that appears to be fairly independent of the diffusion employed. Finally, experiments are conducted in the dry version to see the effects on the kinetic energy spectrum of changing the thermal Rossby number for the simulations." @default.
• W2056520640 created "2016-06-24" @default.
• W2056520640 creator A5003926735 @default.
• W2056520640 creator A5069609564 @default.
• W2056520640 creator A5075772311 @default.
• W2056520640 date "2008-09-24" @default.
• W2056520640 modified "2023-10-13" @default.
• W2056520640 title "Mesoscale spectrum of atmospheric motions investigated in a very fine resolution global general circulation model" @default.
• W2056520640 cites W1972598332 @default.
• W2056520640 cites W1980357988 @default.
• W2056520640 cites W1982342061 @default.
• W2056520640 cites W1987140621 @default.
• W2056520640 cites W2006440391 @default.
• W2056520640 cites W2006986004 @default.
• W2056520640 cites W2008642300 @default.
• W2056520640 cites W2012145501 @default.
• W2056520640 cites W2013069128 @default.
• W2056520640 cites W2014164099 @default.
• W2056520640 cites W2018944558 @default.
• W2056520640 cites W2019004859 @default.
• W2056520640 cites W2025072928 @default.
• W2056520640 cites W2027317184 @default.
• W2056520640 cites W2036624535 @default.
• W2056520640 cites W2038023820 @default.
• W2056520640 cites W2038443410 @default.
• W2056520640 cites W2044000419 @default.
• W2056520640 cites W2050962398 @default.
• W2056520640 cites W2052102312 @default.
• W2056520640 cites W2052989387 @default.
• W2056520640 cites W2059055585 @default.
• W2056520640 cites W2063058023 @default.
• W2056520640 cites W2077789477 @default.
• W2056520640 cites W2078842779 @default.
• W2056520640 cites W2087103831 @default.
• W2056520640 cites W2087713712 @default.
• W2056520640 cites W2092138986 @default.
• W2056520640 cites W2116091942 @default.
• W2056520640 cites W2118729581 @default.
• W2056520640 cites W2126445869 @default.
• W2056520640 cites W2126922865 @default.
• W2056520640 cites W2127525382 @default.
• W2056520640 cites W2140481607 @default.
• W2056520640 cites W2143148027 @default.
• W2056520640 cites W2166456849 @default.
• W2056520640 cites W2168832918 @default.
• W2056520640 cites W2170334105 @default.
• W2056520640 cites W2175830336 @default.
• W2056520640 cites W2178863085 @default.
• W2056520640 cites W2508100462 @default.
• W2056520640 cites W4242015245 @default.
• W2056520640 cites W4254520184 @default.
• W2056520640 doi "https://doi.org/10.1029/2008jd009785" @default.
• W2056520640 hasPublicationYear "2008" @default.
• W2056520640 type Work @default.
• W2056520640 sameAs 2056520640 @default.
• W2056520640 citedByCount "115" @default.
• W2056520640 countsByYear W20565206402012 @default.
• W2056520640 countsByYear W20565206402013 @default.
• W2056520640 countsByYear W20565206402014 @default.
• W2056520640 countsByYear W20565206402015 @default.
• W2056520640 countsByYear W20565206402016 @default.
• W2056520640 countsByYear W20565206402017 @default.
• W2056520640 countsByYear W20565206402018 @default.
• W2056520640 countsByYear W20565206402019 @default.
• W2056520640 countsByYear W20565206402020 @default.
• W2056520640 countsByYear W20565206402021 @default.
• W2056520640 countsByYear W20565206402022 @default.
• W2056520640 countsByYear W20565206402023 @default.
• W2056520640 crossrefType "journal-article" @default.
• W2056520640 hasAuthorship W2056520640A5003926735 @default.
• W2056520640 hasAuthorship W2056520640A5069609564 @default.
• W2056520640 hasAuthorship W2056520640A5075772311 @default.
• W2056520640 hasBestOaLocation W20565206401 @default.
• W2056520640 hasConcept C11111821 @default.
• W2056520640 hasConcept C111368507 @default.
• W2056520640 hasConcept C121332964 @default.
• W2056520640 hasConcept C127313418 @default.
• W2056520640 hasConcept C132651083 @default.
• W2056520640 hasConcept C141452985 @default.
• W2056520640 hasConcept C150284090 @default.
• W2056520640 hasConcept C153294291 @default.
• W2056520640 hasConcept C39432304 @default.
• W2056520640 hasConcept C40382383 @default.
• W2056520640 hasConcept C49204034 @default.
• W2056520640 hasConcept C57879066 @default.
• W2056520640 hasConcept C62279395 @default.
• W2056520640 hasConcept C65440619 @default.
• W2056520640 hasConcept C91586092 @default.
• W2056520640 hasConceptScore W2056520640C11111821 @default.
• W2056520640 hasConceptScore W2056520640C111368507 @default.
• W2056520640 hasConceptScore W2056520640C121332964 @default.
• W2056520640 hasConceptScore W2056520640C127313418 @default.
• W2056520640 hasConceptScore W2056520640C132651083 @default.
• W2056520640 hasConceptScore W2056520640C141452985 @default.
• W2056520640 hasConceptScore W2056520640C150284090 @default.
• W2056520640 hasConceptScore W2056520640C153294291 @default.
• W2056520640 hasConceptScore W2056520640C39432304 @default.
• W2056520640 hasConceptScore W2056520640C40382383 @default.
• W2056520640 hasConceptScore W2056520640C49204034 @default.
• W2056520640 hasConceptScore W2056520640C57879066 @default.

• next