• login
  • register
  • lost your password?

Meteo BCs

  • sitemap
  • mail to me
  • add to bookmarks
  • Home
  • News
  • Programs
  • Support
  • Downloads
  • About us
  • Contacts
  • Home
  • Programs
  • HYDRUS-1D
  • Description
  • References
  • Tutorials
  • Library of Projects
  • Direct
  • Inverse
  • Atmospheric BCs
  • Infiltration
  • Meteo BCs
  • Nonequilibrium Solute Transport
  • Bacteria Transport
  • Nanotube Transport
  • Roots Uptake
  • HP1
  • Unsatchem
  • Portugal
  • Dual-Permeability
  • Centrifuge
  • C-Ride Examples
  • Colloids and Theta Transients
  • Colloid-Facilitated Solute Transport
  • Isotopes
  • Root Growth
  • Freezing/Thawing
  • H1D Overland Flow Module
  • Cosmic Ray Neutron Probe
  • Tillage Mixing
  • HP1 Module
  • UnsatChem Module
  • Package for MODFLOW

Home / Programs / HYDRUS-1D / Library of Projects / Meteo BCs

Hydrus-1D Projects - Meteo

  • Project Group: Meteo
  • Description: Examples demonstrating new options in Hydrus-1D for evaluating atmospheric boundary conditions, including those based on meteorological variables.
  • Availability: Download Test2 examples now (0.8 MB), Download EnBal examples now (1.16 MB), Download Periodic example now (1.07 MB)
Project Description
Test2LAIa This example closely corresponds with the Test2 example from the Direct work group, described in the manual. However, potential values of evaporation and transpiration are calculated internally by HYDRUS using the Bear’s law from entered potential values of evapotranspiration and LAI.
Test2LAIb The same as Test2LAIa, except that daily variations of transpiration and precipitation are generated by HYDRUS.
Test2LAIc The same as Test2LAIa, except that rooting depths are specified.
Test2Met1 Similar as Test2LAIa, except that Potential evaporation and potential transpiration are calculated using the Penman-Monteith combination equation (from solar radiation and other meteorological variables), the rooting depth is specified.
Test2Met2 Similar as Test2LAIa, except that Potential evaporation and potential transpiration are calculated using the Penman-Monteith combination equation (from potential radiation and other meteorological variables), the rooting depth is specified.
EnBal1a Surface energy balance for the experimental site in Riverside, CA, is evaluated based on the input of daily values of solar radiation. Daily variations of meteorological variables are generated using meteorological models.
EnBal1b Surface energy balance for the experimental site in Riverside, CA, is evaluated based on the input of the transmission coefficient and calculated daily potential radiation. Daily variations of meteorological variables are generated using meteorological models.
EnBal1c Surface energy balance for the experimental site in Riverside, CA, is evaluated based on the input of daily values of solar radiation and the transmission coefficient. Daily variations of meteorological variables are generated using meteorological models.
EnBal2a Surface energy balance for the experimental site in Riverside, CA, is evaluated based on the input of hourly values of solar radiation.
EnBal2b Surface energy balance for the experimental site in Riverside, CA, is evaluated based on the input of hourly values of solar radiation and the transmission coefficient.
PMDay Evaporation for the experimental site in Riverside, CA, is evaluated using the Penman-Monteith equation based on the input of daily values of solar radiation. Daily variations of meteorological variables are generated using meteorological models.
Periodic Example demonstrating the use of a set of boundary conditions multiple times. In this particular example, a one year long set (365 d) of BCs is used 5 times.

EnBal examples are based on the experimental data reported by Saito et al. (2006).

  1. Saito, H., J., J. Šimůnek, and B. Mohanty, Numerical analyses of coupled water, vapor and heat transport in the vadose zone, Vadose Zone Journal, 5, 784–800, 2006.

 

Copyright © 2021, PC-Progress s.r.o. | powered by NetGenium