Titlebook: Synoptic-Dynamic Meteorology and Weather Analysis and Forecasting; A Tribute to Fred Sa Lance F. Bosart,Howard B. Bluestein Book 2008 Ameri

Licentious

KIN

Surface Boundaries of the Southern Plains: Their Role in the Initiation of Convective Storms Although some cases of storm initiation along surface boundaries have been well documented using research datasets collected during comprehensive field experiments, much of what we know is based only on empirical forecasting and nowcasting experience. It is suggested that many problems relating to

Ibd810

Strong Surface Fronts over Sloping Terrain and Coastal Plainsw England was initially covered by an unusually warm, dry air mass. Dynamical anticyclogenesis over eastern Canada set the stage for a favorable pressure gradient to allow chilly marine air to approach coastal New England from the east. Diabatic cooling over the chilly (5°–8°C) waters of the Gulf of

Intact

Perspectives on Fred Sanders’ Research on Cold Frontsion, “Frontal structure and the dynamics of frontogenesis.” For a third time in his career, Sanders published several papers (1995–2005) revisiting the structure and dynamics of cold fronts. His 1967 and 1995-2005 work raises the question of the origin and dynamics of the surface pressure trough and

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PTCA635

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Surface Potential Temperature as an Analysis and Forecasting Toolong potential temperature gradients are calculated. The results of the mean potential temperature analyses show that moderate and strong surface baroclinic zones are favored along the coastlines and the slopes of the North American cordillera. Additional subsynoptic details, not found in Sanders and

Intellectual

Dynamical Diagnosis: A Comparison of Quasigeostrophy and Ertel Potential Vorticity can transfer some of their intuition into the Ertel-PV framework. Indeed, many of the differences between pseudopotential vorticity and Ertel potential vorticity are consequences of the choice of definition of quasigeostrophic PV and are not fundamental to the quasigeostrophic system. Thus, at its

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Finescale Radar Observations of a Dryline during the International H2O Project (IHOP_2002)uring a rolling range-height indicator deployment. It was found that there was a secondary (vertical) circulation normal to the easternmost moisture gradient; the circulation comprised an easterly component near-surface flow to the east, a strong upward vertical component in the convergence zone, a

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