Artificial intelligent assistant

geostrophic

answer Answers

ProphetesAI is thinking...

MindMap

Sources

1
geostrophic
geostrophic, a. (dʒiːəʊˈstrɒfɪk) [f. geo- + Gr. στροϕή a turning, f. στρέϕειν to turn + -ic.] Of, pertaining to, or caused by the Coriolis force (see Coriolis); usu. applied to a wind (or a current of water) in which there is a balance between the Coriolis force and the horizontal pressure gradient ... Oxford English Dictionary
prophetes.ai 0.0 3.0 0.0
2
Geostrophic wind
Geostrophic currents Flow of ocean water is also largely geostrophic. Geostrophic approximation Definition of geostrophic wind Geostrophic wind description Fluid dynamics Atmospheric dynamics wikipedia.org
en.wikipedia.org 0.0 1.5 0.0
3
Geostrophic current
Geostrophic flow may be either barotropic or baroclinic. balance and are examples of geostrophic currents. wikipedia.org
en.wikipedia.org 0.0 0.90000004 0.0
4
ageostrophic
ageostrophic, a. Meteorol. (eɪdʒiːəʊˈstrɒfɪk) [f. a- 14 + geostrophic a.] Not geostrophic; spec. designating the wind component which when added to a geostrophic wind gives the actual wind.[1938 R. C. Sutcliffe in Q. Jrnl. R. Meteorol. Soc. LXIV. 502 If there is a general vertical motion in a region... Oxford English Dictionary
prophetes.ai 0.0 0.6 0.0
5
Ageostrophy
Ageostrophy or (ageostrophic flow) is the difference between the actual wind or current and the geostrophic wind or geostrophic current. See also geostrophic geostrophic wind References External links Meteo 422 – Lecture 17 – The Omega Equation Aloft Oceanography fr:Vent géostrophique wikipedia.org
en.wikipedia.org 0.0 0.6 0.0
6
Quasi-geostrophic equations
If the Rossby number is equal to zero then we recover geostrophic flow. The quasi-geostrophic equations were first formulated by Jule Charney. The quasi-geostrophic vorticity equation can be obtained from the and components of the quasi-geostrophic momentum equation which can then be derived wikipedia.org
en.wikipedia.org 0.0 0.3 0.0
7
Frontogenesis
Generally, Rossby number—ratio of inertial to coriolis force is used to formulate a condition of geostrophic flow. To maintain balance, the geostrophic wind aloft and below adjust, such that regions of divergence/convergence form. wikipedia.org
en.wikipedia.org 0.0 0.3 0.0
8
地转流
地转流（geostrophic current） 是一种平行等压线(isobars)的海洋流，是经由海水密度梯度所产生的压强梯度力与科里奥利力平衡时的海流 参考文献 海洋学 洋流 wikipedia.org
zh.wikipedia.org 0.0 0.3 0.0
9
Chinese translation for " quasi-geostrophic approximation
quasi-geostrophic approximation Chinese translation: 准地转近似.... Please click for detailed translation, meaning, pronunciation and example sentences for quasi-geostrophic approximation in Chinese www.translation-dictionary.net
www.translation-dictionary.net 0.0 0.3 0.0
10
Ocean dynamics
Below the mixed layer the upper ocean is generally governed by the hydrostatic and geostrophic relationships. This Ekman transport is superimposed on geostrophic flow associated with horizontal gradients of density. wikipedia.org
en.wikipedia.org 0.0 0.3 0.0
11
地转风
地转风（Geostrophic wind）是一种科氏力和气压梯度力巧妙平衡下产生的一种理论上的风。这个状况称为「地转平衡」。地转风的方向和等压线平行。这种平衡在自然界中很少出现。真正的风几乎总是由地面摩擦力等其他力量产生，与地转风不同。 公式中可能会有其他变数，例如地转风向量可以在恒压表面使用重力位高度 Φ 的形式表示： 参见 地转流 平衡流 盛行风 参考文献 外部连结 Geostrophic approximation Definition of geostrophic wind Geostrophic wind wikipedia.org
zh.wikipedia.org 0.0 0.0 0.0
12
Thermal wind
Examples Advection turning If a component of the geostrophic wind is parallel to the temperature gradient, the thermal wind will cause the geostrophic If geostrophic wind blows from cold air to warm air (cold advection) the geostrophic wind will turn counterclockwise with height (for the northern hemisphere wikipedia.org
en.wikipedia.org 0.0 0.0 0.0
13
Balanced flow
This condition is called geostrophic equilibrium or geostrophic balance (also known as geostrophy). Application Modelers, theoreticians, and operational forecasters frequently make use of geostrophic/quasi-geostrophic approximation. wikipedia.org
en.wikipedia.org 0.0 0.0 0.0
14
Overturning in the Subpolar North Atlantic Program
Geostrophic currents in the basin interior are estimated using temperature and salinity measurements from moorings and gliders. The AMOC is calculated on the basis of the directly measured boundary currents, the geostrophic currents and the Ekman transports estimated from the surface wikipedia.org
en.wikipedia.org 0.0 0.0 0.0
15
Eady model
First, the model assumes the atmosphere is composed of fluid obeying quasi-geostrophic motion. See also Quasi-geostrophic equations Charney Model Cyclogenesis References Holton, James R. Introduction To Dynamic Meteorology 4th Ed. wikipedia.org
en.wikipedia.org 0.0 0.0 0.0