By Robert A. Houze Jr.

ISBN-10: 0080921469

ISBN-13: 9780080921464

ISBN-10: 0123742668

ISBN-13: 9780123742667

As types of the Earth/atmosphere process and observations turn into ever extra refined, and issues approximately weather swap and societal affects of utmost climate and its forecasting develop, realizing the position of clouds within the surroundings is more and more important. Cloud Dynamics, moment Edition provides the basic info had to know the way clouds have an effect on weather and climate.

This complete ebook examines the underlying physics and dynamics of each particular form of cloud that happens within the Earth's surroundings, displaying how clouds fluctuate dynamically counting on whether or not they take place over oceans or mountains, or as components of atmospheric storms, similar to thunderstorms, tropical cyclones, or hot and chilly fronts. protecting either the microphysical and macrophysical facets of clouds, the booklet treats the entire actual scales excited by cloud strategies, from the microscale of the person drops and ice debris as much as scales of storms during which the clouds ensue.

As observational know-how advances with more and more subtle distant sensing services, specific figuring out of the way the dynamics and physics of clouds impact the amounts being measured is of paramount value. This e-book underpins the paintings necessary for right interpretation of those observations, now and sooner or later.

  • Provides the holistic realizing of clouds had to pursue examine on issues important to lifestyles on Earth
  • Provides in-depth knowing of all kinds of clouds over all areas of Earth, from the poles to the equator
  • Includes targeted actual and dynamical perception into the total spectrum of clouds populating Earth's surroundings

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Additional resources for Cloud Dynamics, Second Edition

Sample text

1. 100) The vertical velocity at h is wðhÞ ¼ ht þ uhx , and, if the lower layer is bounded below by a rigid flat surface, wð0Þ ¼ 0. 101) combine to yield the equation 10. This is the case if the upper layer is infinitely deep. 104) Thus, the perturbation in the depth of the lower layer of fluid propagates in the form of a wave of wave number k moving at phase speed c, as the buoyancy force successively restores the depth of the fluid to its mean height at one location and the excess mass is transferred to the adjacent location in x, where a new perturbation is created upon which the buoyancy must act.

A) Stratus and stratocumulus frequency is indicated by fraction of low clouds observed at each grid point that have bases less than 3 km altitude and layer thicknesses less than 3 km. (b) Frequency of moderately deep clouds (most likely moderately deep convective or frontal clouds) seen at each grid point that have bases less than 3 km and layer thicknesses between 3 and 6 km. (c) Frequency of deep clouds (most likely deep convective or frontal clouds) seen at each grid point that have bases less than 3 km and layer thicknesses greater than 6 km.

These clouds include frontal clouds, deep cumulonimbus and mesoscale convective systems. These deep clouds are prominent in both midlatitudes and the tropics—the latitudes where most of Earth’s precipitation falls. The greatest frequency of such clouds is in the equatorial belt, where deep convective clouds are constantly releasing latent heat into Earth’s atmosphere. The equatorial atmosphere with its solar heating and warm oceans favors convective clouds and the tropopause is highest in this part of the atmosphere, which allows the convective clouds to be especially deep.

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