ATMS 411 Homework [Main Page] [Daily Notes] [Final Project]

Homework style example.



Homework 6. Chapter 4.
Turn in this homework assignment through webCampus, prepared using Microsoft Word.

Gain familiarity with geoengineering the Earth's climate.
Use a simple model to understand the role of downwelling infrared radiation on making the planet habitable.
Work with the direct, diffuse, and total radiation reflected and transmitted by clouds, and the role of multiple scattering.

Problem 1

You may copy the problem statement and questions to Microsoft Word and put your answers there.
The Mie theory calculator link will need to be used for this problem.
Here are the class notes for this problem:
Single scattering properties of a single cloud droplet discussion (right click, save, open with OneNote).
Multiple scattering properties of a cloud of droplets discussion (right click, save, open with OneNote).

Problem Statement:
A stratiform cloud fills the sky.
The cloud is 1 km thick, and is a water droplet containing cloud composed of a monodispersion of droplets all having radii = 7 microns.
Assume the droplet single scattering albedo is 1 (no absorption of radiation).
The optical depth at 550 nm is τext=τsca=10, for green light. Note that 550 nm = 0.55 microns.


a. What is the size parameter?

b. What scattering regime is this?

c. What is the scattering efficiency factor? (Mie theory calculator).

d. What is the asymmetry parameter? (Mie theory calculator).
It is also known as the average cosine of the phase function.

e. What is the number concentration of cloud droplets?
[Hint: Calculate this from the given optical depth and the relationship with number concentration.]

f. What fraction of direct sunlight makes it through this cloud?

g. What fraction of total radiation (diffuse and direct) makes it through this cloud?

h. What fraction is the diffuse radiation to the total radiation coming through this cloud?

i. Would the sun be visible when viewed through this cloud? Briefly discuss your answer.
j. What is the liquid water path for this cloud? (total liquid water per unit area).

k. How much water would be collected in a cup of area A swept through the cloud?
(In other words, what is the precipited water in mm, similar to precipitable water vapor).

Resources for Problem 1:
Model to calculate light scattering and absorption by spherical particles, also known as "Mie Scattering" for the person that developed it.

Theory of multiple scattering in one dimension (an excellent discussion).
Single scattering properties of a single cloud droplet discussion (right click, save, open with OneNote).
Multiple scattering properties of a cloud of droplets discussion (right click, save, open with OneNote).



Homework 5
. Chapter 4.
Turn in this homework assignment through webCampus, prepared using Microsoft Word.

Observe how relatively simple analysis can lead to climate insight concerning the Earth's radiatian budget and response time to climate change.

Have a deeper understanding of something we overlook in our daily lives, the blueness of the sky and the polarization of sky light.
Appreciate the radiation deficit from the equator to the poles.

Read chapter 4. The first two problems are related to climate and radiation issues.
1. Do problem 4.21.
Notes on this problem
(right click on link and save to disk. Open with OneNote).
Notes on the problem in PDF format.

2. A. Do problem 4.29. Express your answer for the response time in units of days.
B. Estimate also the response time for the Earth's oceans taken together as one body of water. Express your answer in units of years.
Notes from class on problem discussion.

3. A. What is the ratio of Rayleigh scattering strength for blue light compared with red light by gases in the atmosphere? (You specify wavelengths).
B. How does this affect the color of the sky?
C. Describe the polarization of light seen when looking at 90 degrees from the direction of the sun on a clear day (no clouds or aerosol, just air).
See slides 77-81 and 95-97. Also see this image of the dipole radiation pattern.
If you have polarized sunglasses you can go out and look at the sky at 90 degrees from the sun direction, and rotate the sunglasses to see this effect (don't look directly at the sun!)

4. Do problem 4.56. This problem is intended to help you think about the Earth's radiation budget shown in Figures 4.34 and 4.35.




Chapter 3 and Section 8.3 on deep convection.
1. Turn in this homework assignment through webCampus, prepared using Microsoft Powerpoint.
2. Do an oral presentation in class or through Zoom.

Include a section on the effects of wind and wind shear. Include the Hodograph of your sounding looking for storm direction (winds in first 6 km) and clockwise circulation low followed by straight line later (ref. Vasquez, Instability, skewT and hodograph handbook). Use other indices:
SWEAT Severe weather threat index. Above 300 severe thunderstorm. Above 400 tornados likely. Incorporates thermodynamics (Total Totals) and wind shear.
Total Totals: T850mb + Tdew850mb - 2T500mb. 44-50 General thunderstorms. 51-55 Moderate thunderstorms. 55-59 Strong thunderstorms. 60+ Scattered severe and tornados. CAPE connection. Pg 156 of Vasquez.
Try to find storm relative helicity SRH described on page 158 of Vasquez.


Role of wind shear in severe storm development. Wind shear separates the updraft and downdraft containing precipitation. A horizontal circulation develops, and can be lifted into the vertical, enhancing supercell formation and tornado likelihood. Low LCL and a lot of low level contribution to CAPE also feed severe storms.

Become familiar with soundings that can be associated with severe weather and tornado outbreaks.
Investigate stability of the atmosphere using potential temperature and equivalent potential temperature.
Become familiar with reanalysis data for evaluating previous weather events.
Learn how to obtain and interpret archived radar and infrared satellite imagery.
Practice science communication through giving a presentation.

Preparation: for this homework includes our class discussions, the MetEd module, and reading section 8.3.1a on Deep Convection, pg 344-347 of Wallace and Hobbs.

Steps A-G guide you through acquiring your data and intrepreting it.

A. Find an exciting sounding (using the Univ. of Wyoming site) from anywhere in the continental US, after February 28th, 2017, with a lot of convective available potential energy (CAPE).
Preferably find a sounding that was associated with severe weather in the vicinity.
The limitation on date comes from the availabilty of satellite imagery.
Obtain both the GIF skew T image and the text file.The text file will be used for analyzing the sounding, for graphs and reading values from it.
Color your sounding using the Paint program (or other) to illustrate the level of free convection, equilibrium level,
and regions of positive and negative buoyancy (green for positive, red for negative).
Here's an example.
Check your sounding for issues like these.

I will be using the Reno 3July2021 0Z sounding for the in-class example, so this one is not available for use. Local backup.
Text for the sounding. Local backup.

B. Identify the level of free convection and the equilibrium level.
These can be read from the sounding indices, or at the intersections given by the lifted surface parcel and environmental air.

C. Note and discuss the CAPE, CIN, and precipitable water from your sounding.
Calculate and report the maximum vertical updraft speed in m/s and mph.
wEL=(2CAPE)1/2. Here EL is the equilibrium level.

D. Make a graph of the vertical distribution of potential temperature (THTA in the sounding text) and equivalent potential temperature (THTE in the sounding text).
In your discussion, identify stable, unstable, neutrally stable, and convectively unstable regions.
Here's an example; the top height is at just above the equilibrium level.
Plotting these to just above the equilibrium level (and not the top of the sounding) allows us to see the details in the troposphere.

E. Obtain the 500 mb height map from reanalysis for your sounding for the time of the sounding, and including the location of your sounding.
Here is the link for reanalysis data.
The latitude and longitude range for your graph can be centered at the balloon observation by finding the latitude and longtitude for it, and going +-20 degrees north and south, and west and east for the bounding box.
Interpret in terms of locations of low and high heights, and wind speed maxima and minima.
Here's an example from the 28July2017 0z, Lamont Oklahoma located at about 36.62 North and 97.48 West: Settings and 500 mb plot. Lamont Oklahoma will be in about the center of the image.
Lamont OK is site location 74646.
Draw an arrow showing the 500 mb wind direction at your site (center of the graph) based on the height contour spacings and compare with your sounding wind speed and direction at 500 mb. (Extra credit: do the same with a 700 mb map assignment as well.)

F. Obtain the radar data for your location and its vicinity, and for the time around your sounding.
Use this archived radar data tool and obtain data in and around the time of your sounding.
Radar data can also be obtained from the NOAA Weather and Climate Toolkit described in G.
Here's an example radar movie obtained for the 3 July 2021 0z case study, showing an outflow boundary.

G. Use the NOAA Weather and Climate Toolkit to get an infrared image for the time of your sounding to use in identifying cold cloud tops associated with convection.
We will likely use GOES 16 data for coverage of the entire continentaly U.S., and for better time coverage.
Here's an example of the query. And here is an example image.
The data is "Clean" Infrared Longwave Window Band. The center wavelength for this band is 10.3 microns, or a wavenumber=970.9 cm-1. (wavenumber=1/wavelength).
Estimate cloud top temperature for any convection in the area assuming cloud top is a blackbody radiator.
You can hover over locations of interest and read the infrared radiance.
The measured cloud top radiance can be used with the wavenumber in this calculator to get the brightness temperature. Example calculation.

Introduction: Discuss CAPE and precipitable water vapor amount in the introduction.
Be sure to define each variable when using equations, if you use equations.

Section 1. Use Google Earth and the latitude and longitude coordinates of your sounding to create a map of the location in wide enough of an area to give an idea of its climatological context.
You may find useful climate information on your site here. Describe what motivated you to choose your site.

Section 2. Present your skewT graph and its interpretation, including discussion of the wind speed and direction as a function of height; temperature, and dewpoint temperature; and the lifted air parcel. (See step A).

Section 3. Give a table of values for your location and include:
a. Equivalent potential temperature θE for your air parcel. This value is constant for the entire trajectory of the air parcel lifted from the surface and can be read from the sounding as ThetaE at the LFC.
b. Lifting condensation level height and pressure.
c. Level of free convection in meters and pressure value for it.
d. Tropopause height in meters and the pressure value for it.
e. Equilibrium level height and pressure.
f. Your CAPE value in Joules/kg.
g. Your calculated vertical velocity, w, in meters/second and mph at the equilibrium level based on use of your CAPE value. The equation is w = (2 * CAPE)1/2.
h. Your precipitable water amount in mm units.
i. 500 mb wind direction from the sounding and inferred from the 500 mb level graph.

Section 4. Graph with all the potential temperature and equivalent potential temperature curves versus height.
Discuss atmospheric stability using these graphs. (See step D).

Section 5. Prepare a 500 mb level graph and discuss it. (See step E).

Section 6. Obtain the radar data and discuss it. (See step F).

Section 7. Obtain the infrared satellite image for your area and discuss it. (See step G).

Conclusion: Summarize your findings.

a. You may include any related atmospheric data (like maps of other pressure levels, etc) that helps tell your story.

b. OPTIONAL: 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.
Replace the example sounding with your own and redo the calculations.
(Here's another version; it also has the calculation of the moist adiabatic lapse rate.) I can assist if you would like to work with the program.
You can also make your own program with any language you would like to do this calculation. Explain what program you use, and include it in the report.

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.
3. Historical weather may be obtained here, mostly from surface stations at airports.
4. Archived satellite imagery from around the world can be obtained here.
5. Read section 8.3.1a on Deep Convection, pg 344-347 of Wallace and Hobbs.
6. Skew T plots discussion.
7. Archived weather radar.
8. Ingredients for a thunderstorm.
9. Radar discussion.
10. Thunderstorms.
11. The 500 mb pressure chart.
12. Satellite imagery interpretation in brief.

13. Tornado formation discussion.





Homework 3
. Chapter 3, part 1.
Turn in this homework assignment through webCampus, prepared using Microsoft Word.

Emphasize understanding of the physical quantities used to describe atmospheric thermodynamics.
Relate atmospheric thermodynamics to hurricane dynamics as a real world application.
Practice using the skewT graph and Python programming for atmospheric thermodynamics.

Make one MSword document that has solutions for problems 1 through 4.

Read chapter 3.
1. Define and discuss the following quantities (in your own words. Read about them from various sources and then from memory/understanding, discuss them).
a. Tv virtual temperature
b. Tdew dew point temperature
c. Tw wet bulb temperature
d. θ potential temperature
e. θw wetbulb potential temperature
f. θE equivalent potential temperature

2. Explain in words (no diagram needed) how to use Normand's rule to obtain the following:
a. Dewpoint temperature from the temperature, pressure, and wetbulb temperature.
b. Wetbulb temperature from the temperature, pressure, and dewpoint temperature.

3. Given these values typical for class room air:
Ambient temperature To=21.3 C, wet bulb temperature Tw=12 C and ambient pressure Po=871 mb

a. Skew T diagram showing how Normand's rule, etc, to obtain the quantities listed below, and values entered into the table.
You can copy and paste this table into Microsoft Word and fill it in. You can delete the "Procedure using skewT" column.
Include your skewT diagram showing how you obtained the various quantities as well.

Problem 3 Table: Given To=21.3 C,
wet bulb temperature Tw=12 C and Po=871 mb
Quantity Units Value from skewT Value from Python Comment Procedure using skewT
Tdew C     dewpoint temperature Use Normand's rule
ws(Tdew) g/kg     water vapor mixing ratio at saturation at the dewpoint temperature Read from the skewT
ws(Tw) g/kg     water vapor mixing ratio at saturation at the wetbulb temperature Read from the skewT
ws(T) g/kg     water vapor mixing ratio at saturation at the air temperature Read from the skewT
RH %     Relative humidity RH=ws(Tdew)/ws(T)
θ K     Potential Temperature Follow the dry adiabat through T down to P=1000 mb and read the temperature.
θw K     Wetbulb Potential Temperature Follow the moist adiabat throughTw down to 1000 mb and read the temperature.
θE K     Equivalent Potential Temperature Use Normand's rule to get to the LCL. Then follow the moist adiabat to the top of the atmosphere. Return to 1000 mb along a dry adiabat and read the temperature.
LCL Temperature C     Temperature at the lifting condensation level (LCL) Use Normand's rule
LCL Pressure mb     Pressure at the LCL Use Normand's rule

b. Obtain the dewpoint temperature from this Python program by entering the values of Po, To, and Tw and put it in the table where noted
This program was written for Python 2.7.13. (Add parenthesis around the print statements to make it work for Python 3.x).
You can check the calculation using the National Weather Service water vapor calculator.
The theory for this problem is here.

c. OPTIONAL: Obtain the rest of the table values using this Python program by entering the values of Po, To, and Tdew to the LCL calculator.
This program uses a simple approximation for the equivalent potential temperature, so it's accuracy isn't perfect.
This program was written for Python 2.7.13. (Add parenthesis around the print statements to make it work for Python 3.x).

4. This problem explores hurricane dynamics and thermodynamics.
It will be in short report format as discussed in Homework 2, this time with references.
At the center of a hurricane is a warm core low pressure region, the eye of the hurricane.
This table gives a categorization of hurricanes by maximum wind speed range. (local backup).
a. Discuss the life cycle of hurricanes: formation, energy source, and dissipation (be sure to cite your references, see Resources.) (one paragraph for each, with inline references to the literature you cite/use). Discuss especially ideas/theory for why the eye of the hurricane is mostly clear of clouds, and why the surface wind in the eye wall is so strong.

b. Create a 'hurricane' table with headings Category, Sustained Wind Range (m/s), Eye Pressure Range (mb), Average Eye Temperature Difference (C).
We will use cyclostrophic flow theory in class to show that the pressure difference between the eye and the surroundings is ΔP=1.81ρv2 where ρ is surface density and v is maximum hurricane wind speed. The pressure at the eye of the hurricane is Peye=Po- ΔP. Be sure to convert the units of ΔP to mb.

Use the eye and surrounding pressure to assumed to be 1010 mb to obtain the average temperature difference between the atmospheric column above the eye and surroundings (see prob 3.26).
[We showed that ΔT=Toln(Po/Peye)/ln(Peye/200mb) where To=-3 C = 270 K, and Po=1010 mb.]

Here's an example of the table for the first entry. It's convenient to use Excel for the table.

Hurricane Freddy, Southern Hemisphere 2023, longest lived and most energetic in history.
This paper discusses hurricane properties.
This paper discusses the dynamics of a specific hurricane in detail, including the effect of temperature on hurricane strength.
You can reference it in your report, comparing your values with those in the paper, and find other references for hurricanes using the Web of Science.
We will discuss in class how to use cloud applications for EndNote and WebOfScience to manage references within Microsoft Word (download and install the Endnote plugin for Word).
We did problem 3.26 in class to develop theory for the average column temperature difference and the hurricane eye pressure given the wind speed.
National Hurricane Center site and data.

Numerous websites talk about the circulation in hurricanes.
Hurricane Ian discussion on Tuesday, on Wednesday and on Thursday, September 27-29, 2022.
The powerpoint presentation for chapter 3 may be useful. The hurricane problem is there.


Homework 2
. Chapter 1.
Turn in this homework assignment through webCampus, prepared using Microsoft Word.

NOTE: FUTURE VERSIONS SHOULD CALCULATE THE INTEGRATED VAPOR TRANSPORT as the integral of v rhoWV dz up to 3 or 4 km. It's a good way to become familiar with the concept for Atmospheric River applications.

Study the introductory chapter for an overview of the field.
Access and interpret sounding and reanalysis meteorological data from around the world.
Calculate and graph meteorological variables to investigate their vertical distribution in the atmosphere.
Learn how to make and interpret publication quality graphs for meteorology.
Advance science writing skills.

Make one MSword document that has solutions for problems 1 through 4.

Read chapter 1.
1. Do problem 1.6 parts a, c, d, and i from the textbook. Write your answers into the first part of the MSword document you will be turning in for this assignment.

2. Do problem 1.12 from the textbook, being sure to express your answer in degree C per kilometer.
Then go to the South Pole and find a sounding that best resembles the features of this problem.
Soundings from the South Pole are at Amundsen-Scott station 89009 in Antarctica.
Look at data from perhaps June through August of this year and find a day with cold surface conditions and a strong inversion calculated from the first two points.
You can put the station number 89009 in the website and press enter to access this data.

3. Prepare a short report that describes the atmosphere for 12Z, 3 January 2022 for these two locations, Rochambeau French Guiana (SOCA, Station 81405) and Barrow Alaska USA (PABR, Station 70026) using the high spatial resolution sounding data.
a. Use Google Earth to view these two locations, Rochambeau French Guiana (coordinates 4.8222, -52.3653) and Barrow Alaska USA (coordinates 71.2889, -156.7833). Save images of each location and use as figures 1 and 2 in your report.
Include grid lines in these images so you can see the Tropic of Cancer and the Arctic Circle, respectively, and discuss the significance of these geographical demarcations,
both in of themselves and with respect to the amount of solar radiation expected to be seen seasonally in their vicinity.

b. Acquire the png format skew T soundings for PABR and SOCA for this day and time. Make these soundings figures 3 and 4 in your report.
Discuss these soundings. What is the local standard time at each site for the soundings?
Observe the lapse rate Γ=-dT/dz from the slope of the temperature versus height graph and interpret.

c. Near equator: Rochambeau French Guiana (get sounding text for SOCA from the Wyoming site.)
Plot pressure and temperature vs height as figure 5 in your report.
Calculate density and plot versus height in a separate graph as figure 6).

Density of dry and moist air

d. Near north pole: Barrow Alaska (PABR).
Get the sounding data for PABR from the Wyoming site.
Overlay pressure and temperature vs height with the SOCA pressure and temperature in figure 5.
Calculate density and overlay with the SOCA density in figure 6.

e. Calculate and graph the water vapor density in grams/m3 for Barrow and overlay with the SOCA water vapor density, as an overlay with figure 6.
Note that water vapor density is the product of density * w. Discuss.

f. Then make a graph and fit a trendline for the natural logarithm of pressure, ln(Pressure) vs height
to obtain the scale height of the atmosphere at these two locations,
considering data to a height of 2 km.
Include this graph as figure 7.
Make a table that has the
Calculate the scale height of the atmosphere from the negative reciprocal of the slope.
Use the scale height to calculate the mean virtual temperature of the layer to 2 km.
Calculate the mean virtual temperature of the layer to 2 km also from the sounding.
Compare and discuss these measures of mean virtual temperature.
Here's an example of scale height.

In your report, compare and contrast the difference in the meteorology between these two sites
as a function of height in the atmosphere, both near the surface and throughout the atmosphere.

NOTE: A short report should be written like a short section in a text book.
A. Title for the report. Your name.
B. The first paragraph(s) describes what's in the report, describes what is to be accomplished. References to other literature should be in the name year format, e.g. Smith et. al. 2020.
C. Each figure must have a number and a caption. Figures must be in publication format -- high quality figures with 18 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. Use the equation editor in microsoft word to prepare your equations.
F. The last paragraph should summarize the overall outcome of the report, and possibly discuss your results in comparison with literature results as in part B.
Get started early.
G. List of cited references.
Take advantage of the UNR writing center to have them read your report draft to give you feedback on writing quality.

A. Meteorological data can be obtained from the University of Wyoming web site. Backup of data in case the website is down.
B. Most (or all) computers readily accessible to all students, using their netID, have Google Earth, MSword, and Excel.
C. Students can download office for their home computer. Excel and Word are available for students and faculty here. Sign in with your UNR netID and download Office to your computer. We will import data using the text wizard: Excel:File:Options, then check this box.
D. Description of balloon soundings of the atmosphere.
E. References to published papers and websites can be easily managed with EndNote. Scroll down to "Manage your references" for instructions.

4. a. Do problem 1.21 from the textbook. This is similar to problem 1.20 from the textbook we did in class. The answer is around 2.5 mm⁄sec. Show that the air speed is v=(dp⁄dt) RE ⁄ Ps where RE is Earth's radius and Ps is the average surface pressure. Evaluate the air speed using Python (include in your report).
b. Here are graphs of the surface pressure averaged from 1950 - 2019 for Dec/Jan/Feb and for June/July/August.
[This data is from NCEP/NCAR. One objective of this problem is to become aware of this data].
[Data from NOAA, Physical Science Laboratory, Monthly/Seasonal Climate Composites]. Historical data is available in another form here.
c. Does the pressure distribution support the premise of part a?
d. Discuss the seasonal variation of surface pressure in the Northern hemisphere in summer and winter, locations of highs and lows, and meteorological consequences. (open ended question).
This topic is discussed in this online dynamics textbook near Figure 2.3, the pertinent section is here.
e. Extra Credit: Here are data and graphs for 2020. The data is in netCDF format, and it could be averaged to look at this problem analytically.


Homework 1
Turn in this homework assignment through webCampus, using Microsoft Word, etc.

Skew T lnP Practice homework based on the atmosphere of 17 August 2022 at 12Z chosen at random:
Reno sounding location is 72489 REV (39.56, -119.8). Slidell Louisiana sounding location is 72233 LIX (30.34, -89.83).

Instructions: Place your results from parts 1 through 6
into a Microsoft Word or PDF Document and submit it to Webcampus
You can use OneNote or other programs for doing the homework, just export the assignment as a PDF document.

Download the blank skewT graph to Microsoft Paint, or your favorite image program.

1. From the Reno morning sounding, make a table with the temperature and dewpoint temperature for pressures of mb of 850, 700, 500, 400, and 250 mb. (Local backup).

2. Put these points on the blank skewT graph using Paint, save your skewT image file.

3. Download the actual sounding for the morning, circle the temperature and dewpoint temperature values at the pressures given in part 1. (Local backup).
Compare with your skewT from part 2 with the actual sounding in part 3 to make sure you are understanding these charts.

4. Download the Slidell Louisiana 12Z sounding and discuss the comparison with the Reno sounding. (Local backup).

5. Make a Google Earth map using the coordinates for each location to help your discussion of the meteorology you would expect for Reno and Slidell.

6. What are the local daylight savings and local standard times in Reno and Slidell at the time these soundings?

Some skewT lnP applications and measurements.
Skew T lnP MetEd Module that covers nearly everything, starting with the basics.
How to convert to and from UTC.
Upper air soundings and skewT discussion.



ATMS 411 in class presentation and turn in presentation here.
ATMS 611 in class presentation, report, and turn in presentation here.
Presentations are 5 to 20 minutes long depending on the number of observations and types of data used.

Atmospheric Physics students take photographs and/or use other data of the atmosphere or environment, and explain the Atmospheric Physics connection.
You can use more than one photograph or data source, and can look at a variety of phenomena.
For example, blue sky, sky polarization, coronas, halos, rainbows, lenticular clouds, gravity waves, lightning, water phase clouds, ice phase clouds,
inferring air motions and winds from cloud structures, contrails, vortices in contrails, sky color during pollution events, sky color near the horizon, sky color at sunset looking to the east.
Photographs of the dendritic nature of ice growing on windshields on cold days, the shape and nature of icicles, dew on a moist mornings are also possible topics.
Photographs of snow flakes and snow crystals, here's a discussion.
If you have special hobbies or work, like paragliding, Atmospheric Physics related aspects can be included in your project.
You can use soundings, satellite images, weather station data, etc, to also help tell the story.

ATMS 411 students will do a presentation. Presentation hints. 7 secrets of great speakers. Teachable moments.
ATMS 611 students will do a presentation and a report. Report format.

Due Dates:
Presentations: December 1st by 8 am. Presentations start that day. Turn in your presentation through webCampus.
Reports: December 7th by the end of the day. They can be submitted as a second file through webCampus.

Resources that may help

Gravity wave discussion.
Snow crystal/flake observations.
Cloud identification.
NASA WorldView for satellite imagery. You can add layers for additional information.
National Weather Service balloon soundings, served by the Univ of Wyoming.
Weather station data from the Western Regional Climate Center at DRI. In particular, the UNR weather station.

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