'Trough axis' diaporamas de présentation

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Matthew Cote, Lance Bosart, and Daniel Keyser State University of New York, Albany, NY Michael L. Jurewicz, Sr. Nationa

Matthew Cote, Lance Bosart, and Daniel Keyser State University of New York, Albany, NY Michael L. Jurewicz, Sr. Nationa

Predecessor Rainfall Events (PRE) in Tropical Cyclones - Results from a Recent Northeastern U.S. Collaborative Science, Technology, and Research (CSTAR) Project. Matthew Cote, Lance Bosart, and Daniel Keyser State University of New York, Albany, NY Michael L. Jurewicz, Sr.

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681 views • 55 slides
Matthew Cote, Lance Bosart, and Daniel Keyser State University of New York, Albany, NY

Matthew Cote, Lance Bosart, and Daniel Keyser State University of New York, Albany, NY

Predecessor Rainfall Events (PRE) in Tropical Cyclones - Results from a Recent Northeastern U.S. Collaborative Science, Technology, and Research (CSTAR) Project. Matthew Cote, Lance Bosart, and Daniel Keyser State University of New York, Albany, NY Michael L. Jurewicz, Sr.

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673 views • 55 slides
QG Analysis: Upper-Level Systems

QG Analysis: Upper-Level Systems

QG Analysis: Upper-Level Systems. Will this upper-level trough intensify or weaken? Where will the trough move?. QG Analysis. QG Theory Basic Idea Approximations and Validity QG Equations / Reference QG Analysis Basic Idea Estimating Vertical Motion QG Omega Equation: Basic Form

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596 views • 33 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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475 views • 25 slides
Vertical Cyclone Structure AOS 101 - Section 302 Ross A. Lazear May 1, 2007

Vertical Cyclone Structure AOS 101 - Section 302 Ross A. Lazear May 1, 2007

Vertical Cyclone Structure AOS 101 - Section 302 Ross A. Lazear May 1, 2007. Review. We know that the winds converge at a surface low pressure center and diverge from a surface high pressure center (this is because of the frictional force at the surface)

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385 views • 23 slides
Vertical Cyclone Structure AOS 101 - Section 302 Ross A. Lazear May 1, 2007

Vertical Cyclone Structure AOS 101 - Section 302 Ross A. Lazear May 1, 2007

Vertical Cyclone Structure AOS 101 - Section 302 Ross A. Lazear May 1, 2007. Review. We know that the winds converge at a surface low pressure center and diverge from a surface high pressure center (this is because of the frictional force at the surface)

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384 views • 23 slides
Qualitative Verification of the Operational GFS and Ensemble Mean for 1200 UTC 13 March 2003

Qualitative Verification of the Operational GFS and Ensemble Mean for 1200 UTC 13 March 2003

Qualitative Verification of the Operational GFS and Ensemble Mean for 1200 UTC 13 March 2003. By: Duc Nguyen. Outlines. GFS Initialization for 1200 UTC 13 March 2003 144-Hour Forecast Control Run & Ensemble Mean Plots Spaghetti Plot 240-Hour Forecast Control Run & Ensemble Mean Plots

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201 views • 11 slides

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