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  • ...sigma-coordinate representation shown. [[Mesoscale meteorology|Mesoscale]] models divide the atmosphere vertically using representations similar to the one s ...ctions/technotes/asset-000-000-000-845.pdf|publisher=[[National Center for Atmospheric Research]]|accessdate=2011-01-03|author2=Gall, Robert|author3=Pyle, Matthew ...
    5 KB (663 words) - 10:39, 15 May 2023
  • ...weather prediction]] models for the integration of the equations governing atmospheric motion. A [[Lagrangian and Eulerian specification of the flow field|Lagran It can be shown that the equations governing atmospheric motion can be written in the Lagrangian form ...
    4 KB (543 words) - 03:59, 19 September 2024
  • The '''atmospheric circulation on exoplanets''' refers to the large-scale movement of air mass ...tics, such as [[Rotational frequency|rotation rate]] (fast vs. slow) and [[atmospheric stratification]] (stable vs. unstable), influence circulation patterns. For ...
    8 KB (1,248 words) - 18:09, 16 February 2025
  • {{Short description|Equation in atmospheric chemistry}} ...chanism:<ref name="Barker 1995">{{Cite book|title=Progress And Problems In Atmospheric Chemistry|author=John Roger Barker|publisher=World Scientific|year=1995|isb ...
    4 KB (563 words) - 00:05, 4 May 2023
  • ...ediction|prognostic model forecasts]]. Because of the complexity of these models, forecast verification goes a good deal beyond simple measures of [[associa ...rsistence" forecast]] can still rival even those of the most sophisticated models. An example is: "What is the weather going to be like today? Same as it w ...
    5 KB (705 words) - 17:31, 8 November 2023
  • Trajectories are useful for tracking atmospheric contaminants, such as smoke plumes, and as constituents to [[Lagrangian coo ...ially from a combination of the two, e.g. [[data assimilation|assimilation models]]. ...
    4 KB (532 words) - 08:21, 16 July 2024
  • | title = Atmospheric models for use in hydrodynamic computer codes ...
    1 KB (191 words) - 02:36, 28 March 2023
  • ...d the [[United States Department of Defense]] provide requirements for the models of continuous gusts used in design and simulation of aircraft.<ref name="14 == Models of continuous gusts == ...
    12 KB (1,753 words) - 20:12, 10 September 2023
  • ...d J. |last2=Zeng |first2=Xiping |date=2005-04-01 |title=Modelling tropical atmospheric convection in the context of the weak temperature gradient approximation |u ...title=A Note on Large-Scale Motions in the Tropics |journal=Journal of the Atmospheric Sciences |language=EN |volume=20 |issue=6 |pages=607–609 |doi=10.1175/1520- ...
    13 KB (1,825 words) - 23:27, 5 February 2025
  • ...ref name=":1">{{Cite journal |last=Kajita |first=Takaaki |date=2010 |title=Atmospheric neutrinos and discovery of neutrino oscillations |journal=Proceedings of t ...c neutrinos is different; also, the Waxman-Bahcall bound does not apply to atmospheric neutrinos, but to (ultra)-high-energy neutrinos from outside of our galaxy. ...
    16 KB (2,400 words) - 10:42, 10 February 2025
  • ...sub> and T<sub>s</sub> remain constant over the planet, strong oceanic and atmospheric currents can be imagined to provide plentiful lateral mixing. Furthermore, ...osphere. The remaining fraction (1-ε) is transmitted to space through an [[atmospheric window]]. In the first term on the right, ε is the emissivity of the atmos ...
    16 KB (2,380 words) - 04:29, 21 February 2025
  • ===Atmospheric diffusion and pollutants=== ...alcek, C. J. |title=Effects of wind shear on pollution dispersion |journal=Atmospheric Environment |volume=36 |issue=3 |pages=511–7 |year=2002|bibcode=2002AtmEn.. ...
    15 KB (2,301 words) - 09:01, 29 November 2024
  • The correct result would be ''P'' = 101.325 kPa, the normal (atmospheric) pressure. The deviation is −1.63 kPa or −1.61 %. [[Category:Thermodynamic models]] ...
    3 KB (400 words) - 08:17, 26 August 2024
  • '''Representations of the atmospheric boundary layer in global climate models''' ...ic boundary layer]] (ABL) within [[Global circulation model|global climate models]] (GCMs) are difficult due to differences in surface type, scale mismatch b ...
    12 KB (1,883 words) - 21:42, 14 July 2023
  • ...und |language=en}}</ref> Joe Courtney and John Knaff noted that as several models are based on Atlantic data, it can lead to biases in other parts of the wor Most pressure-wind models are in the form of:<ref name=":0">{{Cite journal |last=Holland |first=Greg ...
    6 KB (894 words) - 04:49, 25 February 2025
  • ...2 - 15% in contrast to the 30 - 40% associated with statistical prediction models.<ref>{{Cite book |last=Final Report |title=Radiowave Propagation Modelling ...be classified as either statistical (S-FS) models or instantaneous (I-FS) models. S-FS are typically empirically-based and relate the attenuation values at ...
    13 KB (1,990 words) - 18:44, 26 August 2024
  • ...ent of inertia]] of the system mantle-crust is only slightly influenced by atmospheric pressure loading, this mainly requires a change in the [[angular velocity]] ...ayer]]. This spin-down time is the characteristic time for the transfer of atmospheric axial angular momentum to Earth's surface and vice versa. ...
    10 KB (1,522 words) - 13:19, 19 February 2025
  • Atmospheric scattering plays a role in removing higher frequencies from direct sunlight [[File:Airmass geometry.png|thumb|Atmospheric effects on optical transmission can be modelled as if the atmosphere is con ...
    22 KB (3,269 words) - 10:14, 8 February 2025
  • In [[atmospheric science]], '''hydrodynamic escape''' refers to a thermal [[atmospheric escape]] mechanism that can lead to the escape of heavier atoms of a [[plan If there is a strong thermally driven atmospheric escape of light atoms, heavier atoms can achieve the escape velocity throug ...
    17 KB (2,519 words) - 05:37, 19 December 2024
  • ...ive observational photometry as well as the use of theoretical atmospheric models.<ref name=":2" /> ...
    4 KB (629 words) - 20:51, 5 July 2024
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