P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming.

Slides:



Advertisements
Similar presentations
Middle Latitude Cyclones
Advertisements

How to “Grow” a Storm Temperature advection is key!
Atmospheric Circulation in a nutshell Hot air rises (rains a lot) in the tropics Air cools and sinks in the subtropics (deserts) Poleward-flow is deflected.
Unit 9: Circulation Patterns of the Atmosphere
Mid-Latitude Cyclones: Vertical Structure
Middle-Latitude Cyclones - II
SO441 Synoptic Meteorology Fronts Lesson 8: Weeks Courtesy: Lyndon State College.
UPPER AIR DYNAMICS (continued) MSC 243 Lecture #8, 10/22/09.
Niels Woetmann Nielsen Danish Meteorological Institute
Midlatitude Cyclones Equator-to-pole temperature gradient tilts pressure surfaces and produces westerly jets in midlatitudes Waves in the jet induce divergence.
Chapter 10 Mid-latitude Cyclones Chapter 10 Mid-latitude Cyclones.
Midlatitude cyclones. Identify and describe the North American air masses that influence the weather patterns for Lexington Differentiate between frontal.
Meteo 3: Chapter 12/13 The Cyclone Model: Common characteristics and evolution of mid- latitude lows Read pages , ,
GEU 0047: Meteorology Lecture 12 Mid-latitude Cyclones.
Extra-Tropical Cyclones and Anticyclones, Chapter 10
Lecture 22: Midlatitude Cyclones (Ch 10) more about divergence its connection with vorticity: the vorticity theorem vorticity plots on the upper charts…
GY205 Weather and Climate Lecture 5 (Please turn in homework on the table)
Jet stream. Jet stream and other upper air winds Jet stream formation Jet stream position Why the jet stream is important –Cyclones.
Class #22: October 20, Class #22: Wednesday, October 20, 2010 Fronts And Extratropical Cyclones.
Fronts and Mid-latitude Cyclones
MET 61 1 MET 61 Introduction to Meteorology MET 61 Introduction to Meteorology - Lecture 12 Midlatitude Cyclones Dr. Eugene Cordero San Jose State University.
Chapter 10: Middle Latitude Cyclones Chapter 10: Mid-latitude Cyclones Most active weather is associated with a cyclone (i.e. low pressure system) Here.
The Midlatitude Cyclone Ahrens, Chapter 12
Gulf of Alaska Noreaster.
Understanding Weather and Climate 3rd Edition Edward Aguado and James E. Burt Anthony J. Vega.
Cyclones and Anticyclones in the Mid-Latitudes
How do the blizzards from?. Review of last lecture Tropical climate: Mean state: The two basic regions of SST? Which region has stronger rainfall? What.
Chapter 10 – Midlatitude Cyclones. The Origin of the Theory of Midlatitude Cyclones The polar front theory (Norwegian cyclone model) – description of.
Weather Patterns.
Chapter 9: Weather Patterns Notes. Maps of Storm Pattern in 1993 Polar-Front Theory (Norwegian Cyclone Model) The middle latitudes – a region between.
The Weather Makers of the Mid-Latitudes
Formation of the Extratropical Cyclone (Cyclogenesis)
The Tricellular Circulation is highly dynamic, varying with the seasons and bringing the Polar front back and forth across the USA. RANGE OF THE POLAR.
Extratropical Cyclones and Anticyclones Chapter 10
Occluded fronts and weather symbols
Middle-Latitude Cyclones - I. RECAP: Types of Fronts Cold fronts: cold, dry stable air is replacing warm, moist unstable air. Moves fast, showers along.
Class #18 Wednesday, February 18, Class #18: Wednesday, February 18 Waves aloft Introduction to Oceanography Ocean Currents.
Chapter 8: Air masses, fronts, and middle-latitude cyclones Air masses Air masses Fronts Fronts Middle-latitude cyclones Middle-latitude cyclones.
Chapter 8: Air Masses, Fronts, and Middle-Latitude Cyclones Air masses Air masses Fronts Fronts Middle-latitude cyclones Middle-latitude cyclones.
Middle Latitude Cyclones This chapter discusses: 1.The location, vertical structure, and developmental stages of middle latitude cyclones 2.How upper level.
Chapter 20.2 Fronts and Lows  Objectives:  -Describe the weather conditions associated with different types of fronts  Describe the life cycle of a.
Today’s Topics Chapter 10 – Extratropical Cyclones and Anticyclones
Announcements Last lab group hand in kits Friday. I have several notebooks left in class. If missing yours, please see me. I will be in my Halloween costume.
Chapter 9: Mid-Latitude Cyclones. Introduction mid-latitude cyclones  produce winds as strong as some hurricanes but different mechanisms contain well.
Air mass source regions and their paths. From C. Donald Ahrens: Essentials of Meteorology: An Invitation to the Atmosphere and D. Miller at UNCA.
Mid-Latitude Cyclones
Class #17 Monday, February 16, Class #17: Monday, February 16 Surface pressure and winds Vertical motions Jet streams aloft.
Recap……. Name the air masses…... Name the weather…..
© 2014 Pearson Education, Inc. Chapter 2 Lecture McKnight's Physical Geography 11e Lectures Chapter 7 Atmospheric Disturbances © 2014 Pearson Education,
UPPER AIR FLOW The height of the atmosphere The height that the atmosphere reaches a certain pressure can tell us information about the air at a certain.
Chapter 6: Weather Systems
Extra-Tropical Cyclones and Anticyclones, Chapter 10
SO254 Extratropical cyclones
Instability Baroclinic instability (needs vertical shear,
AOS 101 Cyclone Structure April 22/24 April 29/May 1.
Atmospheric Lifting Mechanisms
Upper Air Diagrams Dewpoint will be replaced with the dewpoint depression, which is the difference between the temperature and dewpoint. You will not see.
Weather – Air Mass extremely large body of air with similar characteristics of temperature and moisture. Forms when air stagnates for long periods of.
Cyclogenesis in Polar Airstreams
High and Low Pressure Systems Weather Systems Unit
Middle-Latitude Cyclones - II
Air Masses, Fronts, Cyclogenesis
Fronts.
Middle-Latitude Cyclones - I
The Course of Synoptic Meteorology
Chapter 9 Weather Patterns
The Course of Synoptic Meteorology
The Course of Synoptic Meteorology
Extratropical Cyclones Forming East of the Rocky Mountains
Presentation transcript:

p. 277

Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming Stationary front: divides airmasses, but little forward motion Occluded front: cold front “catches up” to warm front warm sector now only found aloft less temperature contrast

Vertical displacement along a cold front

COLD FRONT Infrared Imagery Radar Imagery

Profile of a warm front

Occlusion sequence p. 291

Stationary Front POLAR FRONT POLAR AIRMASS SUBTROPICAL AIRMASS

Maturity

Lifting processes and cloud cover

Occlusion

Convergence and divergence along a Rossby wave

If lows and highs aloft and at the surface are above one another, the systems will weaken !

Divergence aloft promotes the surface low Convergence aloft promotes the surface high Surface divergence Surface convergence

Longwaves

MIGRATE THROUGH THE LONGWAVE TROUGHS

1 2 3 Differential temperature advection intensifies the wave Condensation may release even more heat energy for the storm Less upper level divergence No temp advection

Relative vorticity

Vorticity through a Rossby wave

Values of absolute vorticity on a hypothetical 500 mb map

Temperature variations in the lower atmosphere lead to variations in upper-level pressure

Example of a midlatitude cyclone April 15

April 16

April 18

Flow patterns and large-scale weather – Zonal height patterns “zonal flow”

Meridional flow pattern

Typical winter midlatitude cyclone paths

A. cyclogenesis B. occlusion C. maturity D. senescence What is the term for this early stage in the life cycle of a midlatitude cyclone?

A. cyclogenesis B. occlusion C. maturity D. senescence What is the term for this early stage in the life cycle of a midlatitude cyclone?

A. cyclogenesis B. occlusion C. maturity D. senescence What is the term for this stage in the life cycle of a midlatitude cyclone?

A. cyclogenesis B. occlusion C. maturity D. senescence What is the term for this stage in the life cycle of a midlatitude cyclone?

A. A B. B C. C D. D In which area would overrunning occur? A C B D

A. A B. B C. C D. D In which area would overrunning occur? A C B D

A. A B. B C. C D. D Which location would have the lowest pressure? A C B D

A. A B. B C. C D. D Which location would have the lowest pressure? A C B D

A. 1 B. 2 C. 3 D. 4 Which area would have the greatest positive relative vorticity? [insert figure 10-4]

A. 1 B. 2 C. 3 D. 4 Which area would have the greatest positive relative vorticity? [insert figure 10-4]

A. 1 B. 2 C. 3 D. 4 Which area would have the least relative vorticity?

A. 1 B. 2 C. 3 D. 4 Which area would have the least relative vorticity?

A. uplift over a surface low B. sinking air C. chaotic flow D. anticyclones To what might divergence along the jet stream contribute? [insert figure 10-7]

A. uplift over a surface low B. sinking air C. chaotic flow D. anticyclones To what might divergence along the jet stream contribute?

A. a barotrophic atmosphere B. divergence aloft C. convergence aloft D. negative relative vorticity What would cause this surface low to strengthen? [insert figure 10-11b]

A. a barotrophic atmosphere B. divergence aloft C. convergence aloft D. negative relative vorticity What would cause this surface low to strengthen?

A. A B. B C. C D. D Where is the “dry conveyor belt” in the diagram? B A D C

A. A B. B C. C D. D Where is the “dry conveyor belt” in the diagram? B A D C

A. baroclinic B. zonal C. meridional D. mythical Which term best describes the upper air flow in the diagram?

A. baroclinic B. zonal C. meridional D. mythical Which term best describes the upper air flow in the diagram?

A. baroclinic B. zonal C. meridional D. mythical Which term best describes the upper air flow in the diagram? [insert figure 10-15b]

A. baroclinic B. zonal C. meridional D. mythical Which term best describes the upper air flow in the diagram? insert figure a]