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gfdl's home page > gfdl on-line bibliography > kirsten l. findell > Journal of Hydrometeorology, 4(3), 570-583.

Atmospheric controls on soil moisture-boundary layer interactions. Part II: Feedbacks within the continental United States

Findell, K. L., and E. Eltahir, 2003: Atmospheric controls on soil moisture-boundary layer interactions. Part II: Feedbacks within the continental United States. Journal of Hydrometeorology, 4(3), 570-583.
Abstract: The CTP-HIlow framework for describing atmospheric controls on soil moisture-boundary layer interactions is described in a companion paper, Part I . In this paper, the framework is applied to the continental United States to investigate how differing atmospheric regimes influence local feedbacks between the land surface and the atmosphere. The framework was developed with a one-dimensional boundary layer model and is based on two measures of atmospheric thermodynamic properties: the convective triggering potential (CTP), a measure of the temperature lapse rate between approximately 1 and 3 km above the ground surface, and a low-level humidity index, HIlow. These two measures are used to distinguish between three types of early-morning atmospheric conditions: those favoring moist convection over dry soils, those favoring moist convection over wet soils, and those that will allow or prevent deep convective activity, independent of the surface flux partitioning.
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last modified: March 23 2004.