S. S. Vaidya, V. N. Lykossov, S. S. Singh. 1993: Effect of Counter-Gradient in the Computation of Turbulent Fluxes of Heat and Moisture in a Regional Model. Adv. Atmos. Sci, 10(1): 85-94., https://doi.org/10.1007/BF02656956
Citation:
S. S. Vaidya, V. N. Lykossov, S. S. Singh. 1993: Effect of Counter-Gradient in the Computation of Turbulent Fluxes of Heat and Moisture in a Regional Model. Adv. Atmos. Sci, 10(1): 85-94., https://doi.org/10.1007/BF02656956
S. S. Vaidya, V. N. Lykossov, S. S. Singh. 1993: Effect of Counter-Gradient in the Computation of Turbulent Fluxes of Heat and Moisture in a Regional Model. Adv. Atmos. Sci, 10(1): 85-94., https://doi.org/10.1007/BF02656956
Citation:
S. S. Vaidya, V. N. Lykossov, S. S. Singh. 1993: Effect of Counter-Gradient in the Computation of Turbulent Fluxes of Heat and Moisture in a Regional Model. Adv. Atmos. Sci, 10(1): 85-94., https://doi.org/10.1007/BF02656956
Effect of Counter-Gradient in the Computation of Turbulent Fluxes of Heat and Moisture in a Regional Model
The counter-gradient terms in the computations of turbulent fluxes of heat and moisture have been included in the PBL parameterization of a regional model for monsoon prediction. Results show that inclusion of counter-gra-dient terms has a marginal impact in the prediction of large scale monsoon circulation and rainfall rates.