By John M. Wallace, Peter V. Hobbs
Wallace and Hobbs' unique variation of Atmospheric technological know-how 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 newest discoveries and applied sciences, and get ready themselves for extra complex learn and real-life challenge fixing.
Atmospheric technological know-how, moment variation, has been thoroughly remodeled by way of content material and visual appeal. It comprises new chapters on atmospheric chemistry, the Earth system,climate, and the atmospheric boundary layer, in addition to more advantageous therapy of atmospheric dynamics, climate forecasting, radiative move, critical storms, and human affects, akin to international warming. The authors illustrate strategies with colourful state of the art imagery and canopy an enormous volume 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 factors, and broad updates, Wallace & Hobbs' Atmospheric technological know-how, moment version, is the basic first step in instructing today's atmospheric scientists.
Full-color satellite tv for pc imagery and cloud pictures illustrate ideas all through
Extensive numerical and qualitative workouts emphasize the applying of easy 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 historical past of meteorology
Companion site encourages extra complicated exploration of textual content themes: supplementary info, pictures, and bonus exercises.
Read Online or Download Atmospheric Science: An Introductory Survey (2nd Edition) PDF
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Additional resources for Atmospheric Science: An Introductory Survey (2nd Edition)
Due to the dome-like shape of the ice sheets and the plasticity of the ice itself, the compressed layers of ice gradually creep downhill toward the periphery of the ice sheet, causing the layer as a whole to spread out horizontally and (in accordance with the conservation of mass) to thin in the vertical dimension. 01 Permafrost 5 a 1 Surface area is expressed as percentage of the area of the surface of the Earth. Mass is expressed in units of 103 kg mϪ2 (numerically equivalent to meters of liquid water) averaged over the entire surface area of the Earth.
A. Knauss, Introduction to Physical Oceanography, 2nd Edition, p. 2, © 1997. ] 1 The small effect of pressure upon density is taken into account through the use of potential density, the density that a submerged water parcel would exhibit if it were brought up to sea level, conserving temperature and salinity. ) 2 Ice floats on lakes because the density of fresh water decreases with temperature from 0 to 4 °C. In contrast, sea ice floats because water rejects salt as it freezes. 5 27 0 28. 0 5 26.
The NADW and AABW, each marked by its own distinctive range of temperatures and salinities, are Fig. 3 Vertical sounding of water temperature and salinity in a vertical sounding in the subtropical Atlantic Ocean. Numbers along the sounding indicate depths in hundreds of meters. , pressure-adjusted) density (in o͞oo) is indicated by the contours. Characteristic temperature and salinity ranges for North Atlantic deep water (NADW) and Antarctic bottom water (AABW) are indicated by shading. [Reprinted from Seawater: Its Composition, Properties and Behavior, The Open University in association with Pergamon Press, p.
Atmospheric Science: An Introductory Survey (2nd Edition) by John M. Wallace, Peter V. Hobbs