Rossby parameter

Rossby parameter

The Rossby parameter is a number used in geophysics and meteorology which arises due to the northward variation of the Coriolis force caused by the spherical shape of the Earth. It is important in the generation of Rossby waves.

The Rossby parameter eta is given by the equation:

:eta = frac{1}{a} frac{d}{dphi} (2 omega sinphi) = frac{2omega cosphi}{a} [ [http://amsglossary.allenpress.com/glossary/search?id=rossby-parameter1 Glossary of Meteorology] , American Meteorological Society.] [ [http://mesolab.meas.ncsu.edu/~linyl/mea713/Ch1_Note.doc Lecture Notes] for Atmospheric Science Mesoscale Dynamics (MEA 713). North Carolina State University. Accessed 14 July 2007.]

Where phi is the latitude, omega is the angular speed of the Earth's rotation, and a is the mean radius of the Earth.

Although both involve Coriolis effects, the Rossby parameter describes the "variation" of the effects with latitude (hence the latitudinal derivative), and should not be confused with the Rossby number.

References


Wikimedia Foundation. 2010.

Игры ⚽ Нужен реферат?

Look at other dictionaries:

  • Rossby wave — Rossby (or planetary) waves are giant meanders in high altitude winds that are a major influence on weather. Their emergence is due to shear in rotating fluids, so that the Coriolis force changes along the sheared coordinate. In planetary… …   Wikipedia

  • Rossby-Zahl — Die Rossby Zahl (Ro und nicht R0, nach Carl Gustaf Rossby) ist eine dimensionslose Kennzahl, die vorwiegend in der Geophysik bei ozeanografischen und atmosphärischen Phänomenen Verwendung findet. Sie gibt den Einfluss der Erdrotation an, das… …   Deutsch Wikipedia

  • Rossby-Wellen — Rọssby Wellen   [nach C. G. A. Rossby],    1) Meereskunde: großräumige Meereswellen, deren rücktreibende Kraft aus räumlichen Änderungen des Verhältnisses von Coriolis Parameter (Coriolis Kraft) und Wassertiefe resultiert. Rossby Wellen stellen… …   Universal-Lexikon

  • Rossby radius of deformation — In atmospheric dynamics and oceanography, the Rossby radius of deformation is the length scale at which rotational effects become as important as buoyancy effects in the evolution of the flow about some disturbance. : L {R} equiv frac{NH}{f {0,… …   Wikipedia

  • Carl-Gustaf Rossby — Carl Gustaf Arvid Rossby (Stockholm 28 December, 1898 ndash; Stockholm 19 August, 1957) was a Swedish U.S. meteorologist who first explained the large scale motions of the atmosphere in terms of fluid mechanics.Rossby came into meteorology and… …   Wikipedia

  • climate — /kluy mit/, n. 1. the composite or generally prevailing weather conditions of a region, as temperature, air pressure, humidity, precipitation, sunshine, cloudiness, and winds, throughout the year, averaged over a series of years. 2. a region or… …   Universalium

  • Coriolis effect — For the psychophysical perception effect, see Coriolis effect (perception). Classical mechanics Newton s Second Law …   Wikipedia

  • Balanced flow — In atmospheric science, balanced flow is an idealisation of atmospheric motion. The idealisation consists in considering the behaviour of one isolated parcel of air having constant density, its motion on a horizontal plane subject to selected… …   Wikipedia

  • Cnoidal wave — US Army bombers flying over near periodic swell in shallow water, close to the Panama coast (1933). The sharp crests and very flat troughs are characteristic for cnoidal waves. In fluid dynamics, a cnoidal wave is a nonlinear and exact periodic… …   Wikipedia

  • Poincare-Welle — Die Poincaré Welle, benannt nach Henri Poincaré (1854–1912), ist wie die Kelvinwelle eine Flachwasserwelle in einem rotierenden Bezugssystem. Inhaltsverzeichnis 1 Eigenschaften 2 Vorkommen und Beobachtungen 3 Mathematische Beschreibung 3.1… …   Deutsch Wikipedia

Share the article and excerpts

Direct link
Do a right-click on the link above
and select “Copy Link”