NWP (Meteo 526) Project 2

Parameterization Types Chosen

Boundary LayerMilena Borissova
Ryan Cutter
Bob Much (focus on land surface)
Deep ConvectionPat Maloit
Neil McGillis
Jon Radkovich
Cirrus CloudsMatt Boehm

Guidelines for Project 2

  • I encourage team work in this project. Based on the table above, I envisage two groups: (a) Boundary layers Much, Borissova and Ryan; and (b) Clouds Boehm, McGillis, Radkovich and Maloit.
  • Team work fits most naturally in background discussions and the presentations. Your written papers should be individual efforts, but should have benefited from much group interaction.
  • Project 2 will be assessed in three ways: (i)an initial presentation of the basic theory of the parameterization being studied; (ii)a follow-up presentation on your plans for an exciting, forward-looking parameterization of this general type (which may, or may not, choose to build on the one you have described); (iii)a short written paper on your parameterization-of-the-future.
  • Please settle upon your parameterization papers as soon as possible (Friday this week!). We need to begin scheduling talks, so that we meet the end of semester deadline. The project deadline may be slipped back.

  • NWP (Meteo 526) Project 2 Assessment Guidelines

    Presentation Expectations

  • Presentations will be professional, that is, they will require some thought. Don't expect to stand up and do them without planning.
  • Presentations will last 15-20 minutes per paper with extra time for questions and discussion. I expect to complete 2 papers per class period in which we do this.
  • Since this project is meant to combine team and individual work, you may choose to combine your presentations. Two folks (time limits numbers) may discuss a pair of parameterizations that have similar theoretical underpinnings. You can split the discussion up as you like.
  • The first presentation should be used to describe an existing parameterization: (i) its range of applicability; (ii)its underlying assumptions; (i) the theoretical model on which it builds; (iv)examples of its use; (v) shortcomings you see. This is a huge amount of ground to cover in 15-20 minutes, so see me if you want help in whittling the content down to the essentials.

  • Paper Expectations

  • The paper should focus specifically on your plans for a state-of-the-future parameterization. Feel free to assume that you live in a utopia of unlimited funding resources (although try to keep within the current bounds of data available). Go wild!
  • Paper content should include your basic assumptions, major ways in which they differ from earlier work, discussion of evidence that this will produce improvements and/or justification for making the attempt in this way.
  • The paper will be a formal, conference style paper of only 3-4 pages.
  • If you must exceed this page limit you may, but it will not necessarily improve your grade by adding volume.


    Dates for Initial Project 2 Presentations

    These presentations are to provide the basis of your forays into parameterization improvements. Thus, you will explain the underlying assumptions for the parameterizations you have chosen and their advantages and/or faults. There need be no clear winners or losers. See above for more information.

    Monday13 AprilBob Much (thanks Bob!)
    Wednesday15 AprilPat Maliot
    Jon Radkovich
    Friday17 AprilMatt Boehm
    Neil McGillis
    Monday20 AprilMIDTERM EXAM
    Wednesday22 AprilMilena Borissova
    Ryan Cutter


    Motivation for Project 2 Papers and Second Presentations

    In the paper and these final presentations you need to sell your ideas on parameterization improvements. Picture yourself among a group of collaborators with whom you are planning to write a joint proposal. The money is there, but you have to convince your colleagues that your ideas are exciting and time is short!. In 15 minutes, you must capture their imaginations and swing them over to your way of thinking on this topic, or you'll end up having to follow "Deadly Fred's" tried and true method . You must explain your ideas for the parameterization improvements you advocate or justify scuppering the old scheme (Deadly Fred's favorite!) in favor of starting a new system from scratch.


    Classes Through End of Semester

    Friday24 April Discussion resulting from first talks; Paper due
    Monday27 AprilBob Much; Reviews of each other's first paper versions
    Wednesday29 AprilPat Maliot
    Jon Radkovich
    Neil McGillis
    Friday1 MayMatt Boehm
    Milena Borissova
    Ryan Cutter
    FINAL version of paper due in


    Discussion Topics for Class, Friday 24 April

    Should we expect a unique solution between cloud or boundary layer structure and large-scale averages of other variables? If we could observe a number of different situations on the fine scale, is it possible/likely that they could have the same large-scale averaged quantities? Think of examples for/against this possibility.
    If large-scale averages do not determine the subgrid-scale structure uniquely, this pulls the rug out from under the basic premise of parameterization! How could we design an experiment to determine the uniqueness of a solution?
    Alternatively, is there any way to determine whether an overriding driving toward some new balance (as all stability related parameterizations do) is all that is required for a successful and realistic simulation, since most widely-used parameterizations have been shown to remain within the bounds of reality?
    Is there a relative scale dependence in your answers? i.e. does the definition of "large-scale" and "subgrid-scale" determine the outcome?
    Is using one model to validate another an appropriate approach? If so, should any constraints be placed on how/when this is done?
    Since there are data available describing the atmosphere, should the onus be on the modelers to find a way to use these data to validate their models? One example is that details of clouds are tough to get, but have been obtained for many specific cases. From these we can calculate Q1 (apparent heating) and Q2 (apparent moistening) over some larger area average and validate against these. Beware, I have just led you back to the first discussion topic above!


    Return to general discussion of Project 2. Back to the main class homepage.


    Last Updated: 22 April 1998