The Sverdrup Balance The steady, linear vorticity equation was found to be (2) The Sverdrup balance 3V = Curl()), where upper case symbols indicate depth-integrated velocities, is obtained by

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Jim Shuttleworth 1Center for Sustainability of semi‐Arid Hydrology and Riparian Areas (SAHRA), Department of Hydrology and Water Resources, University of Arizona, Tucson, AZ, USA 2Joint Centre for

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• Evaporation
• Water cycle
• Water vapor
• Water balance
• Penman equation
• Hydrology
• Water
• Atmospheric sciences

Technical Report No. 39 REFERENCE EVAPOTRANSPIRATION WITH RADIATIONBASED AND TEMPERATURE-BASED METHODS - IMPACT ON HYDROLOGICAL DROUGHT USING WATCH FORCING DATA Lieke A. Melsen, Henny A.J. van Lanen, Niko Wanders,

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• Leaf Area Index
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Supplement of Hydrol. Earth Syst. Sci. Discuss., 12, 4271–4314, 2015 http://www.hydrol-earth-syst-sci-discuss.netdoi:hessdsupplement © Author(sCC Attribution 3.0 License.

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Reference and Tutorial Manual An Introduction to Biochemical Modeling using JDesigner

Source URL: sbw.kgi.edu

• Science
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• Mass balance
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Source URL: hycom.org

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Source URL: hycom.org

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