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Download e-book for iPad: Atmospheric Processes and Systems (Routledge Introductions by Russel Thompson

By Russel Thompson

ISBN-10: 0415171458

ISBN-13: 9780415171458

Atmospheric approaches and platforms offers a concise creation to the ambience and the basics of climate. interpreting diversified elements of the mass, power and circulate platforms within the surroundings, this article presents targeted bills of particular phenomena, together with* the composition and constitution of the ambience* power transfers* the cycle of atmospheric water by way of evaporation, condensation and precipitation* strain and winds on the basic or international scale* secondary air plenty and fronts* thermal transformations and climate disturbances.The textual content comprises 16 boxed case reviews, annotated additional examining lists and a word list of key words.

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Additional info for Atmospheric Processes and Systems (Routledge Introductions to Environment Series)

Sample text

Chapter 5 explains the functioning and roles of the ELR and emphasises that it is indeed a highly variable rate and it can be steepened or inverted on a regular basis. e. constant temperatures) well into the lower stratosphere. Indeed, this stable cloudless zone a few kilometres above the tropopause provides ideal flying conditions for supersonic jet airliners like Concorde. 1) to reach 0 °C at 50 km (at the stratopause). This reversal of the normal ELR represents a significant inversion of temperature and is associated with the zone of maximum ozone concentration.

2 kg m-3. 3 In fact, a column of air from the Earth’s surface to the top of the atmosphere exerts a pressure that is equivalent to a column of water 11 m high or mercury 760 mm high. 4 This is the reason why mercury barometers (see Chapter 9) are the most realistic and accurate way of measuring variations in atmospheric pressure. 5 Atmospheric pressure decreases with height at a rate of 6 cm 1000 m-1, since it depends on the weight of the air above it. 2 kg m-3). 1) based on the thermal properties of the atmosphere, although they are not separated with equal degrees of sharpness and do not occur at fixed elevations.

Is reduced due to the reduced albedo (typically 5–10 per cent lower) of the urban fabric. /LW? fluxes over the urban area, which are counterbalanced again to produce small overall changes. For example, the urban heat island has high rates of emissivity (see equation (8)) and outgoing LW? radiation. However, this loss is counterbalanced by large amounts of incoming LW? radiation (averaging 11 per cent more over Hamilton, Canada) associated with the enhanced greenhouse effect (see Chapter 3, Case Study) in polluted urban/industrial air (with increased CO2 and water vapour concentrations).

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