Encyclopedia of Physical Science and Technology, Volume 2Academic Press, 1992 - Physical sciences |
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Page 257
... wind ( G ) , and assume as boundary conditions that the wind is zero at the surface , but approaches the geostrophic value at a large distance above the ground . These boundary conditions essentially describe friction against the ground ...
... wind ( G ) , and assume as boundary conditions that the wind is zero at the surface , but approaches the geostrophic value at a large distance above the ground . These boundary conditions essentially describe friction against the ground ...
Page 301
... winds is proportional to wind speed and increases with increasing roughness . In the surface layer , σ „ and u are independent of height . * พ increases , When convection increases , σw / U eventually becoming proportional to ( z / L ) ...
... winds is proportional to wind speed and increases with increasing roughness . In the surface layer , σ „ and u are independent of height . * พ increases , When convection increases , σw / U eventually becoming proportional to ( z / L ) ...
Page 412
... wind magnetic field lines . The small inset shows a part of the electric current circuit that is generated by the solar wind - magneto- sphere dynamo . since it consists of charged particles , mainly protons and electrons . As the solar ...
... wind magnetic field lines . The small inset shows a part of the electric current circuit that is generated by the solar wind - magneto- sphere dynamo . since it consists of charged particles , mainly protons and electrons . As the solar ...
Contents
Guide to Using the Encyclopedia ix Atomic Physics | 339 |
Approximations and Expansions 1 Atomic Spectrometry | 357 |
Archaeological Geology 31 Atomic Spectroscopy | 381 |
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