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- The '''atmospheric circulation on exoplanets''' refers to the large-scale movement of air masses on planet ...slow) and [[atmospheric stratification]] (stable vs. unstable), influence circulation patterns. For example, a planet's rotation rate can determine whether its a ...8 KB (1,248 words) - 18:09, 16 February 2025
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- ...ard N.|title=Available Potential Energy and the Maintenance of the General Circulation|journal=Tellus|date=May 1955|volume=VII|issue=2|pages=157–167|doi=10.1111/j Any atmospheric circulation system, whether it is a small-scale [[weather]] system or a [[Prevailing wi ...4 KB (637 words) - 11:56, 30 May 2022
- The '''atmospheric circulation on exoplanets''' refers to the large-scale movement of air masses on planet ...slow) and [[atmospheric stratification]] (stable vs. unstable), influence circulation patterns. For example, a planet's rotation rate can determine whether its a ...8 KB (1,248 words) - 18:09, 16 February 2025
- {{Short description|Quantity associated with atmospheric waves}} ...e Northern Hemisphere, wavenumbers 1 and 2 are important for the time-mean circulation due to topography ([[Tibetan Plateau]] and [[Rocky Mountains]]),<ref>{{cite ...3 KB (458 words) - 07:15, 30 December 2024
- The applications of geophysical fluid dynamics do not generally include the circulation of the [[mantle (geology)|mantle]], which is the subject of ''[[geodynamics [[Ocean circulation]] and [[air circulation]] are typically studied in oceanography and meteorology. ...10 KB (1,377 words) - 02:47, 23 February 2025
- ...kert|first2=H.|last3=Ziemianski|first3=M. J.|year=2003|title=The Bjerknes' Circulation Theorem: A Historical Perspective|url=https://elib.dlr.de/9916/1/03-hv.pdf| ===Circulation=== ...12 KB (1,936 words) - 11:29, 16 June 2024
- ...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
- ...into the atmosphere because of its reduced solubility, acting to increase atmospheric carbon dioxide by 6.5[[permille|‰]]. This is thought to partly offset the n ...onal overturning circulation]] (MOC) through the slowing of [[thermohaline circulation]]. Increased stratification means that there is effectively a barrier to su ...7 KB (996 words) - 18:30, 26 November 2024
- ...the associated [[Meridional overturning circulation|Meridional Overturning Circulation]] (MOC). ...overline{\psi} </math>) rotates clockwise and counteracts the eddy induced circulation (<math> \psi* </math>) which rotates counterclockwise.'']]Dynamics in the S ...14 KB (1,903 words) - 11:08, 15 January 2024
- ...MP...63..899R |url=https://zenodo.org/record/1233963}}</ref> and [[general circulation model]]s of the atmosphere allow high precision determination of changes in ...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
- ...ey K. Atmospheric and oceanic fluid dynamics: fundamentals and large-scale circulation. Cambridge University Press, 2006.</ref> ...3 KB (520 words) - 19:52, 20 February 2025
- '''Representations of the atmospheric boundary layer in global climate models''' ...lanetary boundary layer|atmospheric boundary layer]] (ABL) within [[Global circulation model|global climate models]] (GCMs) are difficult due to differences in su ...12 KB (1,883 words) - 21:42, 14 July 2023
- In early and low powered engines with hopper cooling there is little circulation. Water is instead slowly boiled off, with the [[heat of vaporisation]] need ...that the hopper does not boil dry, the temperature cannot exceed the 100°C atmospheric boiling point of water. This is both an advantage and a disadvantage: it ma ...7 KB (984 words) - 06:36, 14 August 2023
- ...ed studies using three dimensional [[Ocean general circulation model|ocean circulation models]], confirming the existence of multiple equilibria in the AMOC. {{Main|Atlantic meridional overturning circulation}} ...24 KB (3,492 words) - 16:03, 12 January 2025
- ...37-6}}.</ref><ref name="Goody Yung 1989">Goody, R.M., Yung, Y.L. (1989). ''Atmospheric Radiation. Theoretical Basis'', second edition, Oxford University Press, Ne ...}, page 250.</ref><ref name="WH 2006">Wallace, J.M., Hobbs, P.V. (2006). ''Atmospheric Science: An Introductory Survey'', 2nd edition, Elsevier, Amsterdam, {{ISBN ...16 KB (2,277 words) - 18:19, 4 September 2024
- ...png|thumb|Dark zones are regions of weak inertial stability in atmospheric circulation.]] ...ore | title= Mesoscale Processes | publisher= [[University Corporation for Atmospheric Research|UCAR]] | accessdate= August 23, 2019 | date= 2001 | pages= 10–53 | ...14 KB (2,139 words) - 18:10, 12 August 2023
- ...the sill.<ref name=":2" /> Processes like mixing, [[Circulation (physics)|circulation]] and [[convection]] contribute to these pressure gradients. The overflow v ...to an anticyclonic regime takes place on an interannual timescale, but the atmospheric forcing also shows a seasonal cycle. During summer the weakened cyclonic wi ...20 KB (2,846 words) - 08:40, 18 January 2024
- ...pical Cyclones. Part I: Steady-State Maintenance| journal = Journal of the Atmospheric Sciences| volume = 43| issue = 6| pages = 585–605| year = 1986| last1 = Ema ...e = Dissipative heating and hurricane intensity| journal = Meteorology and Atmospheric Physics| volume = 65| issue = 3–4| pages = 233–240| year = 1998| last1 = Bi ...15 KB (2,207 words) - 10:40, 5 November 2024
- ...Ocean–Atmosphere System. Part II: Nonlinear Cases |journal=Journal of the Atmospheric Sciences |language=EN |volume=48 |issue=10 |pages=1238–1248 |doi=10.1175/15 ...0-01 |title=El Niño—The Dynamic Response of the Equatorial Pacific Oceanto Atmospheric Forcing |journal=Journal of Physical Oceanography |language=EN |volume=5 |i ...23 KB (3,674 words) - 18:00, 4 October 2024
- ...rd f plan?|date=September 2024}} the lowest-order balance for quasi-steady circulation at higher latitudes.<ref>Pedlosky, J., [https://books.google.com/books?id=F ...st=Pedlosky |first=J. |author-link=Joseph Pedlosky |year=1996 |title=Ocean Circulation Theory |publisher= Springer |edition=2nd |isbn=978-3-540-60489-1 |no-pp=yes ...11 KB (1,639 words) - 13:02, 29 January 2025
- {{Short description|Mixing of seawater at different depths by mesoscale ocean circulation and large, strong winds}} ...omena that controls the intensity of the [[Atlantic Meridional Overturning Circulation]] (AMOC).<ref name=":1">{{Cite journal|last1=Kovalevsky|first1=D. V|last2=B ...26 KB (3,962 words) - 19:23, 5 January 2025