ATMS 411 Homework [Main Page] [Daily Notes]

 

Homework style example.
Homework style example with a graph.

ONLINE ASSIGNMENTS ARE GIVEN IN WEBCAMPUS.

TEAMS FOR HOMEWORK ASSIGNMENTS WHEN REQUIRED.
Team Korian:
Tayebeh, Mohammed, Bin
Team Crafty: Shawn, Chris, Mason
Team Cirrus: Zac, Fiona, Taylor
Team Rock and Ice:
Sean, Abby, Cameron
Team Purple Bears: Brandon, Kylyn, Bradley
Team Isobars: Stormi, Travis, Amanda, Kegan
Team A-Team: Sam, Dylan, Elise
Team Greased Lightning: Jacob, Christian, Grzeborz
Team F-sharp minor: Yuta, Maxwell, Thomas

Homework 3. Each team will do a report and a presentation for the following. (One report and presentation from each team).

1. For each team member, find an exciting sounding from anywhere and anytime in the world (using the Univ. of Wyoming site) with a lot of convective available potential energy (CAPE).
a. Identify the level of free convection and the equilibrium level.

b. Using the sounding text, calculate the CAPE in units of Joules/kg, the estimated vertical velocity at the equilibrium level in meters/second and compare with the value on the sounding.
Also, calculate the precipitable water vapor amount in units of mm and compare with the values given on the sounding.
This spreadsheet will help you calculate temperature along the moist adiabat and gives an example for CAPE and precipitable water calculation.
(Here's the updated version we worked on in class; it also has the calculation of the moist adiabatic lapse rate.)

c. Make a graph of the vertical distribution of potential temperature (THTA in the sounding text) and equivalent potential temperature (THTE in the sounding text).
These graphs will look like the height vs temperature graphs we did in homework assignment 1.
In your discussion, identify stable, unstable, and neutrally stable regions.
Here's an example from our Barrow, Rochambeu study; however, just make your plot to the equilibrium level.
Also, just plot the data for THTA and THTE in the sounding, not the model curves.
Potential temperature and equivalent potential temperature for summer in Barrow and Rochambeau.


d. Obtain the 500 mb height map from reanalysis for your sounding, or from the University of Wyoming, for the time of the sounding, and including the location of your sounding.
Here is the specific link to use for obtaining it from reanalysis.
Interpret in terms of locations of low and high heights, and wind speed maxima and minima.
Here's an example from the 28July2017 0z sounding location, Lamont Oklahoma located at about 36.7 North and 97.6 West: Settings and 500 mb plot. Lamont Oklahoma will be in about the center of the image.

Report:
In the report, each team member will be listed as a coauthor.
The goal is to make your report as short as possible, but to include everything.
Introduction: Discuss CAPE and precipitable water vapor amount in the introduction, and discuss the importance of each. Be sure to define each variable when using equations.

Section 1. Include the skewT graph from the Univ of Wyoming and its interpretation. One figure for each team member.

Section 2. Give a table of values for your locations and include values in your table for:
a. Equivalent potential temperature θE for your air parcel (from the spreadsheet). This value is constant for the entire trajectory of the air parcel lifted from the surface.
b. Lifting condensation level height and pressure.
c. Level of free convection in meters and pressure value for it.
d. Equilibrium level height and pressure.
e. Your calculated CAPE value in Joules/kg.
f. Your calculated vertical velocity in meters/second at the equilibrium level based on use of your CAPE value.
g. Your precipitable water amount in mm.
Use one table with data from all team members.

Section 3. Prepare one graph with all the potential temperature and equivalent potential temperature curves versus height for each team member, to compare them.
You may need to have one graph for potential temperature, and one for equivalent potential temperature if they get too busy to put all on a single graph.
Discuss atmospheric stability in terms of these graphs.

Section 4. Prepare one 500 mb level graph for each team member. Discuss.

Conclusion: Summarize your findings.

Appendix: Optional extra credit. You may include any related atmospheric data (like archived radar data, maps of other pressure levels, etc) that helps tell your story.

Presentation:
Each team member will explain their own skewT graph.
One team member can do the section 2 discussion.

Tools and Extras
1. Soundings from the University of Wyoming site.
2. You may also obtain archived data for the 500 mb level, and precipitation data from radar imagery here.

 

 

 

 

 

Homework 2. Read chapter 3. Do problems 3.18, 3.20, 3.23, 3.26 (also discussed in class), 3.28.
(it will be helpful to read problems 3.21 and 3.22 before doing 3.23).
Note: Not all of the online solutions for the latter problems are correct, especially 3.23.
Be sure to take notes during presentations of homework problems, as this will help you complete the assignment.

Here are the Team Presentation Assignments: Each student will present part or all of a problem (everyone pitches in).
Team Korian: Present problems 3.18a, b, c
Team Crafty: Present problems 3.18d, e, f
Team Cirrus: Present problems 3.18g, h, i
Team Rock and Ice: Present problems 3.18j, k, l
Team Purple Bears: Present problems 3.18m, n, o
Team Isobars: Present problems 3.18p, q, r
Team A-Team: Present problems 3.18s, t, u
Team Greased-Lightning: Present problems 3.18v, w, and 3.20
Team F-sharp minor: 3.23, 3.26, 3.28

 

 

 

Homework 1. Turn in this homework assignment through webCampus.
Read chapter 1.
A. Do problem 1.6. Write your answers into the first part of the MSword document you will be turning in for this assignment.
B. Prepare a short report using Google Earth, MSword, and Excel to explore the following:

Meteorology of the world: Use Google Earth to view these two locations, Rochambeau French Guiana and Barrow Alaska USA.
Look at data for 12Z, 24 January 2017
Near equator: Rochambeau French Guiana (get sounding for SOCA from the Wyoming site, plot pressure and temperature vs height, calculate density and plot versus height)
Near north pole: Barrow Alaska (get sounding for PABR from the Wyoming site, plot pressure and temperature vs height, calculate density and plot versus height)
Then fit a trendline for ln(Pressure) vs height to obtain the scale height of the atmosphere at these two locations, considering data to a height of 2 km.
Observe the lapse rate Γ=-dT/dz from the slope of the temperature versus height graph and interpret.
Compare and contrast the difference in the meteorology between these two sites for 24 January 2017.
Graduate students, also discuss the difference in meteorology between these two sites for 24 August 2017 that we did in class (undergrads can do so for extra credit).

NOTE: A short report should be written like a short section in a text book.
A. Title for the report. Your name.
B. First paragraph describes what's in the report, describes what is to be accomlished.
C. Provide figures, each figure with a number and caption. Figures must be in publication format -- high quality figures with 16 point (or greater) bold black font; tick marks inside. All axes 1 point thick and black.
D. Each figure must be discussed in the text by number, describing the significance of the figure and its relationship to other figures as needed.
E. Any equations should be offset, as in a textbook, and each equation should have a number. Refer to equations by number.
F. The last paragraph should summarize the overall outcome of the report.
Get started early. Take advantage of the UNR writing center to have them read your report draft to give you feedback on writing quality.

TOOLS:
A. Meteorological data can be obtained from the University of Wyoming web site.
B. Most (or all) computers readily accessible to all students, using their netID, have Google Earth, MSword, and Excel.
C. You can use your netID to also access these software packages through the UNR remote services application.

 

 

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