geostrophic การใช้

• In the free atmosphere, geostrophic wind relationships should be used.
• Balance between these two forces is referred to as geostrophic.
• In other words, no vertical wind shear of the geostrophic wind.
• Unlike geostrophic currents, and geostrophic winds are examples of inertial waves.
• Unlike geostrophic currents, and geostrophic winds are examples of inertial waves.
• GOCE mapped the deep structure of the Earth's geostrophic ocean currents.
• The Navier Stokes equations applied to atmospheric motion can be simplified by geostrophic approximation.
• Flow of ocean water is also largely geostrophic.
• Geostrophic flow may be either barotropic or baroclinic.
• This Ekman transport is superimposed on geostrophic flow associated with horizontal gradients of density.
• They follow the principle of geostrophic winds.
• The geostrophic reversed in April to a strong eastward jet spanning the whole equatorial Pacific.
• Dynamically these nearly geostrophic turbulent eddies are the oceanographic counterparts of the atmospheric synoptic scale.
• This is known as geostrophic flow.
• The effect of friction, between the air and the land, breaks the geostrophic balance.
• Isallobaric gradients are important components of the wind as they increase or decrease the geostrophic wind.
• Below the mixed layer the upper ocean is generally governed by the hydrostatic and geostrophic relationships.
• This is called geostrophic balance, and is equivalent to saying that the Rossby number is small.
• The geostrophic wind component is the result of the balance between Coriolis force and pressure gradient force.
• Geostrophic currents in the basin interior are estimated using temperature and salinity measurements from moorings and gliders.