Titlebook: Cold Region Atmospheric and Hydrologic Studies. The Mackenzie GEWEX Experience; Volume 1: Atmospheri Ming-ko Woo Book 2008 Springer-Verlag

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978-3-642-09320-3Springer-Verlag Berlin Heidelberg 2008

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Wolf-Dieter Schleuning,Robert L. Medcalfnto the Basin, (2) interactions of the large-scale atmospheric flows with physical environment of the Basin and their effect on its weather and climate, and (3) application of research results to climate issues in the Basin and beyond.

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Leonard Annetta,Stephen C. Bronackclouds but will lead to biases in inferred cloud thickness and multi-layering. State-of-the-art operational models tend to produce too much high cloud but too little surface precipitation due to sublimation and evaporation rates being too high.

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Irregular Ring Even Edge Flexagons,3. The result suggests that the snow amount depends roughly linearly on the 850 hPa temperature with a correlation coefficient of 0.62. The snowfall-temperature relationship can be used to complement the Quantitative Precipitation Forecast (QPF) available from operational NWP models.

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Working with Documents—Records and Streamsl trajectories were identified that originated near the Gulf of Mexico and terminated over the southern MRB. The transport time ranged from 6 to 10 days. Our study indicates that rapid lee cyclogenesis over Alberta (associated with a 500-hPa cutoff low) and the Great Plains Low Level Jet can act in unison to produce this moisture transport.

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