Land Cover and the Climate System View Full Text


Ontology type: schema:Chapter     


Chapter Info

DATE

2003

AUTHORS

R. W. A. Hutjes , P. Kabat , A. J. Dolman

ABSTRACT

The earth’s land-cover and vegetation interact with the atmosphere by several inter-linked mechanisms (Figure 4.1). Vegetation controls evaporation through its internal physiology: the opening of stomata responds to environmental conditions such as temperature, humidity deficit, radiation, CO2 concentration, and soil moisture. The opening of the stomata also affects the rate of photosynthesis. Stomata respond rather quickly to changes in environmental conditions. A characteristic time scale for coupling with the atmosphere is typically 0.01–1 hrs (strong coupling). More passively, through radiative properties and aerodynamic characteristics, vegetation affects partitioning of the surface energy balance and also dynamics of the wind. Although the coupling between these surface characteristics (e.g., albedo, roughness) is determined by very fast, turbulent processes (typical time scales in seconds), a significant change in albedo would normally follow the seasonal evolution of vegetation with time scales of a week to a year (moderate coupling). More... »

PAGES

73-110

Book

TITLE

Global Environmental Change and Land Use

ISBN

978-90-481-6308-3
978-94-017-0335-2

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/978-94-017-0335-2_4

DOI

http://dx.doi.org/10.1007/978-94-017-0335-2_4

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1026861888


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