Lesson 1:
Diagnosing Synoptic Scale Internal Forcing: Using Potential Vorticity in Operations
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Description |
This lesson shows you the benefits of using Potential Vorticity to help you diagnose vertical motions induced by short-wave troughs in the mid- to upper-troposphere. The author, Phil Schumacher, SOO NWS FSD, shows you how to use tropopause pressure maps to infer vertical motion using models whose resolution precludes you to use Q-vectors. |
Estimated Lesson Completion Time |
40 min. |
Module Type |
Articulate Presenter Module
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| Resources |
Exercises |
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Review Sheets & Hand Outs |
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Lesson Links |
NOAA employees should access this module via the NWS Learning Center as they will need to complete the exam and survey in the LMS to receive credit for completion. All others wishing to take this lesson should use the follow link(s):
IC 5.1: Using Potential Vorticity in Operations
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Lesson 2:
Diagnosing Mesoscale Internal Forcing: Frontogenesis
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Description |
We certainly cannot have a winter weather warning course without a lesson on frontogenesis. Phil Schumacher (SOO NWS FSD) and Dr. Dave Schultz (Research Scientist at CIMMS/NSSL) provide information on frontogenesis starting with some theory and then application to a few cases. This is an important lesson that may help clarify your understanding of this important precipitation forcing mechanism. |
Estimated Lesson Completion Time |
25 min. |
Module Type |
Articulate Presenter Module
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| Resources |
Exercises |
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Review Sheets & Hand Outs |
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Lesson Links |
NOAA employees should access this module via the NWS Learning Center as they will need to complete the exam and survey in the LMS to receive credit for completion. All others wishing to take this lesson should use the follow link(s):
IC 5.2: Diagnosing Mesoscale Internal Forcing: Frontogenesis
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Lesson 3:
The Effect of Stability on the Response of internal forcing in the Atmosphere
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Description |
Stability modulates how the atmosphere responds to precipitation forcing. However, the various combinations of inertial and gravitational stability that the atmosphere creates can often be confusing. This lesson provides you an understanding of how inertial and gravitational stability can combine to yield slantwise instability, and the proper methods to diagnose stability. Phil Schumacher and Dave Schultz team up again to help firm up your ideas on atmospheric stability. |
Estimated Lesson Completion Time |
35 min. |
Module Type |
Articulate Presenter Module
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| Resources |
Exercises |
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Review Sheets & Hand Outs |
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Lesson Links |
NOAA employees should access this module via the NWS Learning Center as they will need to complete the exam and survey in the LMS to receive credit for completion. All others wishing to take this lesson should use the follow link(s):
IC 5.3: The Effect of Stability on the Response of Internal Forcing in the Atmosphere
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Lesson 4:
Examples of Frontal Precipitation Bands
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Description |
While the theory on frontogenesis was provided to you in lesson 2, Mike Evans, SOO NWS BGM, takes that theory and shows you how frontogenesis manifests itself in a variety of cases across the country. Be ready for an informative journey that will help you expand your working memory of how frontogenesis appears in a variety of conditions. |
Estimated Lesson Completion Time |
30 min. |
Module Type |
Articulate Presenter Module
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| Resources |
Exercises |
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Review Sheets & Hand Outs |
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Lesson Links |
NOAA employees should access this module via the NWS Learning Center as they will need to complete the exam and survey in the LMS to receive credit for completion. All others wishing to take this lesson should use the follow link(s):
IC 5.4: Examples of Frontal Precipitation Bands
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Lesson 5:
Structure of Trowals
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Description |
Even though the concept of a TROWAL is not new, it has gained favor recently because it provides a good explanation for observed precipitation patterns in extratropical cyclones. Dr. Pat Market (Univ. of Missouri, Columbia) helps explain how fundamental precipitation forcing mechanisms manifest themselves in a TROWAL. Dr. Market also shows you several ways to diagnose TROWALS, each diagnosis method being better than the previous. |
Estimated Lesson Completion Time |
30 min. |
Module Type |
Articulate Presenter Module
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| Resources |
Exercises |
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Review Sheets & Hand Outs |
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Lesson Links |
NOAA employees should access this module via the NWS Learning Center as they will need to complete the exam and survey in the LMS to receive credit for completion. All others wishing to take this lesson should use the follow link(s):
IC 5.5: Structure of Trowals
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Lesson 6:
Cool-Season Orographic Precipitation processes and Prediction
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Description |
Here is a lesson on topographic forcing of precipitation authored by Dr. Mike Meyers (SOO NWS GJT), Dr. Doug Wesley (COMET), and Dr. W. James Steenburgh (Univ. of Utah). You will see three sections: the first covering the dynamics and microphysics representative of all orographic precipitation, the second dealing with the behavior of topographic precipitation for several mountain ranges in the western US, and the final section on methods and tools for forecasting orographic precipitation. Parts of this lesson are contributions from the COMET module titled "Dynamics and Microphysics of Cool-Season Orographic Storms" while other parts represent new findings. This is an optional lesson but if you do have even the most subtle orographic effects, you will find this lesson valuable. |
Estimated Lesson Completion Time |
50 min. |
Module Type |
Articulate Presenter Module
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| Resources |
Exercises |
IC5 lesson 6 job sheet |
Review Sheets & Hand Outs |
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Lesson Links |
NOAA employees should access this module via the NWS Learning Center as they will need to complete the exam and survey in the LMS to receive credit for completion. All others wishing to take this lesson should use the follow link(s):
IC 5.6: Cool-Season Orographic Precipitation Processes and Prediction
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Description |
Tom Niziol (MIC, NWS BUF) delivers an entertaining and informative overview of lake effects, or more generally, precipitation forcing through localized diabatic heating. You will learn many aspects of lake effect, from quantifying temperature and moisture modification by using the Philip's equations within BUFKIT to understanding enlarged band morphology using high resolution ETA model output. |
Estimated Lesson Completion Time |
25 min. |
Module Type |
Articulate Presenter Module
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| Resources |
Exercises |
IC 5 Lesson 7 job sheets. |
Review Sheets & Hand Outs |
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Lesson Links |
NOAA employees should access this module via the NWS Learning Center as they will need to complete the exam and survey in the LMS to receive credit for completion. All others wishing to take this lesson should use the follow link(s):
IC 5.7: Lake Effects
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