Download Atmospheric Science: An Introductory Survey (2nd Edition) by John M. Wallace, Peter V. Hobbs PDF

By John M. Wallace, Peter V. Hobbs

Wallace and Hobbs' unique variation of Atmospheric technology helped outline the sphere approximately 30 years in the past, and has served because the cornerstone for many college curriculums. Now scholars and pros alike can use this up-to-date vintage to appreciate atmospheric phenomena within the context of the most recent discoveries and applied sciences, and get ready themselves for extra complex research and real-life challenge fixing.

Atmospheric technology, moment variation, has been thoroughly remodeled by way of content material and visual appeal. It includes new chapters on atmospheric chemistry, the Earth system,climate, and the atmospheric boundary layer, in addition to improved remedy of atmospheric dynamics, climate forecasting, radiative move, serious storms, and human affects, resembling international warming. The authors illustrate thoughts with colourful state of the art imagery and canopy an enormous quantity of latest info within the box. they've got additionally built a number of on-line fabrics for teachers who undertake the text.

With its thorough assurance of the basics, transparent causes, and wide updates, Wallace & Hobbs' Atmospheric technology, moment version, is the basic first step in teaching today's atmospheric scientists.

Full-color satellite tv for pc imagery and cloud pictures illustrate ideas all through
Extensive numerical and qualitative routines emphasize the appliance of simple actual ideas to difficulties within the atmospheric sciences
Biographical footnotes summarize the lives and paintings of scientists pointed out within the textual content, and supply scholars with a feeling of the lengthy heritage of meteorology
Companion site encourages extra complicated exploration of textual content themes: supplementary info, photos, and bonus exercises.

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Additional resources for Atmospheric Science: An Introductory Survey (2nd Edition)

Example text

Most of the density gradient tends to be concentrated within a layer called the pycnocline, which ranges in depth from a few tens of meters to a few hundred meters below the ocean surface. The density gradient within the pycnocline tends to inhibit vertical mixing in the ocean in much the same manner that the increase of temperature with height inhibits vertical mixing in atmospheric temperature inversions and in the stratosphere. In particular, the pycnocline strongly inhibits the exchange of heat and salt between the mixed layer, which is in direct contact with the atmosphere, and the deeper layers of the ocean.

Chapter 10 revisits some of these same topics in the context of climate dynamics, with a quantitative discussion of feedbacks and climate sensitivity. 1 Components of the Earth System This section introduces the cast of characters and briefly describes their roles and interrelations in the ongoing drama of climate. The atmosphere, which in some sense plays the starring role, has already been introduced in Chapter 1. The interplay between atmospheric radiation and convection regulates the temperature at the Earth’s surface, setting the limits for snow and ice cover and for the various life zones in the biosphere.

25 are manifestations of these oceanic storm tracks. Rainfall data shown in Fig. 4 What’s Next? 21 48N 46N 44N 42N 40N 38N 36N 34N 32N 124W 122W 120W 118W 116W 114W 122W 110W 108W 106W 104W 102W 100W 2 5 8 10 12 16 20 30 40 60 80 100 Fig. 26 Annual-mean precipitation over the western United States resolved on a 10-km scale making use of a model. The color bar is in units of inches of liquid water (1 in. 54 cm). Much of the water supply is derived from a winter snow pack, which tends to be concentrated in regions of blue, purple, and white shading.

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