Model help:TopoFlow-Meteorology: Difference between revisions

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Revision as of 12:29, 4 May 2011

The CSDMS Help System

TopoFlow-Meteorology

The module is the meteorology process component for a D8-based, spatial hydrologic model

Model introduction

This component reads a variety of variables for the atmosphere and for the land surface from input files or as simple scalars. It then computes many additional variables, such as vapor pressure, eair, and net shortwave (solar) radiation, QnSW, using built-in [shortwave radiation] and [longwave radiation] calculators that are based on celestial mechanics and widely-used empirical relationships. These additional variables are needed by the Snowmelt → Energy Balance and Evaporation → Energy Balance components. Direct, diffuse and back-scattered radiation fluxes are all modeled. Properties of the atmosphere (e.g. precipitation rate, P, air temperature, Tair, relative humidity, RH, and dust attenuation, γ), are used as well as surface/topographic properties (e.g. slope angle, aspect angle and surface albedo. The approach used here closely follows the one outlined in Appendix E of Dingman (2002)[1]. However, instantaneous vs. day-integrated radiation fluxes are used and the optical air mass is modeled using the widely used method of Kasten and Young (1989)[2].

Model parameters

Parameter Description Unit
Components status Enabled/Disabled
Input directory
Output directory
Site prefix file prefix for the study site
Case prefix file prefix for the model scenario
Number of steps number of time steps
Time step meteorology time step sec
ρ H2O type allowed input types (Scalar/Grid/Time_Series/Grid_Sequence)
ρ H2O density of water kg/m3
Cp_air type allowed input types (Scalar/Grid/Time_Series/Grid_Sequence)
Cp air heat capacity of air J/kg/K
ρ_air type: allowed input types (Scalar/Grid/Time_Series/Grid_Sequence)
ρ air density of air kg/m3
Precipitation rates type allowed input types (Scalar/Grid/Time_Series/Grid_Sequence)
Precipitation rates mm/yr
PRECIPITATION ONLY toggle toggle to turn off all variable updates except precipitation
Parameter Description Unit
First parameter Description parameter [Units]
Parameter Description Unit
First parameter Description parameter [Units]
Parameter Description Unit
First parameter Description parameter [Units]
Parameter Description Unit
First parameter Description parameter [Units]

Uses ports

This will be something that the CSDMS facility will add

Provides ports

This will be something that the CSDMS facility will add

Main equations

  • Absolute optical air mass equation
[math]\displaystyle{ m_{abs} \left ( \gamma \right ) = \rho _{0} \int _{0} ^ \infty \left ( \rho / \rho _{0} \right ) \{ 1 - [ 1 + 2 \delta _{0} \left ( 1 - \rho / \rho _{0} \right ) ] \ast [ \cos \gamma / \left ( 1 + h / R \right ) ] ^2 \} ^ {\frac{-1}{2}} dh }[/math] (1)
[math]\displaystyle{ m \left ( \gamma \right ) = m _{abs} \left ( \gamma \right ) / m_{abs} \left ( 90^o \right ) }[/math] (2)

Notes

  • Note on input parameters

For each input variable, you may choose from the droplist of data types. For the "Scalar" data type, enter a numeric value with the units indicated in the dialog. For the other data types, enter a filename. Values in files must also use the indicated units.

Single grids and grid sequences are assumed to be stored as RTG and RTS files, respectively. Time series are assumed to be stored as text files, with one value per line. For a time series or grid sequence, the time between values must coincide with the timestep provided.

For DEMs with pixel geometry and bounding box given in terms of Geographic coordinates, the latitude and longitude of each pixel is used in the calculations. For DEMs with a "fixed-length" pixel geometry (e.g. UTM coordinates), which tend to span smaller areas, the dialog prompts for a single lat/lon pair to be used in the calculations.

  • Note on Equations

time zone:Boundaries of time zones can be very irregular and a time zone map should be consulted if you are unsure. The time zone is not simply a function of the longitude. You can select an adjacent time zone to include the effect of Daylight Savings Time. Time zones with non-integer offsets from GMT are not yet supported.

slope:Topographic slopes (not slope angles) are specified as dimensionless numbers [m/m]. A RiverTools grid (RTG file) with extension "_slope.rtg", "_mf-slope.rtg" or "_dinf-slope.rtg" can be used.

aspect:Aspect is specified as an angle measured in radians counter-clockwise from due east (the standard convention). A RiverTools grid (RTG file) with extension "_mf-angle.rtg" or "_dinf-angle.rtg" can be used for the (continuous-angle) aspect grid.

QSW is set to zero between the times of local sunset and local sunrise, so frames in the RTS file that correspond to nighttime hours will contain only zeros.

Examples

An example run with input parameters, BLD files, as well as a figure / movie of the output

Follow the next steps to include images / movies of simulations:

See also: Help:Images or Help:Movies

Developer(s)

Scott Peckham

References

Dingman, S.L (2002) Physical Hydrology, 2nd ed., Prentice Hall, New Jersey. (see Appendix E)

Kasten and Young (1989) Revised optical air mass tables and approximation formula. Applied Optics, 28 (22): 4735~4738. (for the optical air mass equation)

Liston, G. *******

Marks and Dozier (1992) ******* Water Resources Research.

Whitman, A.M. (2003) A simple expression for the equation of time, online document, http://www.sunspot.noao.edu/sunspot/pr/answerbook/expl-5.html

Links

  1. Dingman, S.L (2002) Physical Hydrology, 2nd ed., Prentice Hall, New Jersey. (see Appendix E)
  2. Kasten and Young (1989) (for the optical air mass equation)