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Extratropical Cyclones and Anticyclones Chapter 10

Extratropical Cyclones and Anticyclones Chapter 10

Extratropical Cyclones and Anticyclones Chapter 10. case study the jet stream and upper-level divergence low-level cyclogenesis synergy between upper-level trof and surface low the life cycle of a frontal disturbance air parcel trajectories. the Edmund Fitzgerald. 9 Nov 1975.

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1.15k views • 50 slides
Flow Channeling in the Mohawk & Hudson Valleys

Flow Channeling in the Mohawk & Hudson Valleys

Flow Channeling in the Mohawk & Hudson Valleys. A FURTHER INVESTIGATION OF MOHAWK HUDSON CONVERGENCE. Tenth Annual Northeast Regional Operational Workshop/NWS/CESTM. Hugh W Johnson IV Lance F. Bosart Michael E. Augustyniak. Geography of New York & New England.

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540 views • 42 slides
Mid-Latitude Cyclones: Vertical Structure

Mid-Latitude Cyclones: Vertical Structure

Mid-Latitude Cyclones: Vertical Structure. Lecture 13 CASE STUDY DUE NEXT WEEK!. Review. Extratropical cyclones generally first develop along an intersection of two airmasses (like a stationary front)

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481 views • 25 slides
Air mass source regions and their paths.

Air mass source regions and their paths.

Air mass source regions and their paths. . From C. Donald Ahrens: Essentials of Meteorology: An Invitation to the Atmosphere and D. Miller at UNCA. Cold Front. Cold Front Cross-Section. Possible Conditions Near a Cold Front. Warm Front. Warm Frontal Cross-Section.

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1.37k views • 23 slides
Predictability and dynamical processes Heini Wernli Institute for Atmosphere and Climate Science ETH Zurich HIW Workshop

Predictability and dynamical processes Heini Wernli Institute for Atmosphere and Climate Science ETH Zurich HIW Workshop

Predictability and dynamical processes Heini Wernli Institute for Atmosphere and Climate Science ETH Zurich HIW Workshop, Karlsruhe 18 March 2013. Key points the dynamics of high-impact weather is often complex and closely related to basic/fundamental research questions,

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286 views • 17 slides
The formation of surface circulation systems

The formation of surface circulation systems

The formation of surface circulation systems. (Bluestein, pp. 213-214). Given an upper-level, positive PV anomaly is advected over a zone of strong, low-level, north-south horizontal temperature gradient:. As for an upper-trough moving over a zonally-oriented surface cold front

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176 views • 6 slides

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