A Parameterization Scheme Accounting for Nonhydrostatic Effects on the Momentum Flux of Vertically Propagating Orographic Gravity Waves: Formulas and Preliminary Tests in the Model for Prediction Across Scales (MPAS)

• Published in: Journal of the atmospheric sciences Vol. 81; no. 5; pp. 805 - 817
• Main Authors: Xu, Xin, Zhang, Rongrong, Teixeira, Miguel A. C., van Niekerk, Annelize, Xue, Ming, Lu, Yixiong, Xue, Haile, Li, Runqiu, Wang, Yuan
• Format: Journal Article
• Language: English
• Published: Boston American Meteorological Society 01.05.2024
• Subjects: Anisotropy; Atmospheric circulation; General circulation models; Gravity wave drag; Gravity waves; Lower stratosphere; Mathematical models; Momentum; Momentum flux; Momentum transfer; Momentum transport; Mountains; Northern Hemisphere; Numerical models; Orographic gravity waves; Parameterization; Physics; Plateaus; Simulation; Southern Hemisphere; Stratosphere; Surface water waves; Surface waves; Troposphere; Upper troposphere; Wave drag; Wave power; Wave propagation; Weather; Wind; Winter
• ISSN: 0022-4928; 1520-0469
• DOI: 10.1175/JAS-D-23-0020.1

The momentum transport by orographic gravity waves (OGWs) plays an important role in driving the large-scale circulation throughout the atmosphere and is subject to parameterization in numerical models. Current parameterization schemes, which were originally developed for coarse-resolution models, commonly assume that unresolved OGWs are hydrostatic. With the increase in the horizontal resolution of state-of-the-art numerical models, unresolved OGWs are of smaller horizontal scale and more influenced by nonhydrostatic effects (NHE), thus challenging use of the hydrostatic assumption. Based on the analytical formulas for nonhydrostatic OGWs derived in our recent study, the orographic gravity wave drag (OGWD) parameterization scheme in the Model for Prediction Across Scales is revised by accounting for NHE. Global simulations with 30-km horizontal resolution are conducted to investigate NHE on the momentum transport of OGWs and their impacts on the large-scale circulation in boreal winter. NHE are evident in regions of complex terrain such as the Tibetan Plateau, Rocky Mountains, southern Andes, and eastern Antarctica. The parameterized surface wave momentum flux can be either reduced or enhanced depending on the relative importance of NHE and model physics–dynamics interactions. The NHE corrections to the OGWD scheme significantly reduce the easterly biases in the polar stratosphere of the Northern Hemisphere, due to both weakened OGWD in the upper troposphere and lower stratosphere and suppressed upward propagation of resolved waves into the stratosphere. However, the revised OGWD scheme only has a weak influence on the large-scale circulation in the Southern Hemisphere during boreal winter.