TL;DR: In this paper, the authors examined the spatio-temporal patterns of atmospheric carbon dioxide transport predicted by the Regional Atmospheric Modeling System (RAMS) and found that using the Exner function has a substantial impact on the spatial pattern of carbon dioxide predicted by RAMS.
Abstract: This paper examines the spatio-temporal patterns of atmospheric carbon dioxide transport predicted by the Regional Atmospheric Modeling System (RAMS). Forty-eight hour simulations over northern New England incorporating a simple representation of the diurnal summertime surface carbon dioxide forcing arising from biological activity indicate that, in its native formulation, RAMS exhibits a significant degree of mass non-conservation. Domain-wide rates of non-physical mass gain and mass loss are as large as three percent per day which translates into approximately eleven parts per million per day for carbon dioxide - enough to rapidly dilute the signature of carbon dioxide fluxes arising from biological activity. Analysis shows that this is due to the approximation used by RAMS to compute the Exner function. Substitution of the exact, physically complete equation improves mass conservation by two orders of magnitude. In addition to greatly improving mass conservation, use of the complete Exner function equation has a substantial impact on the spatial pattern of carbon dioxide predicted by the model, yielding predictions differing from a conventional RAMS simulation by as much as forty parts per million. Such differences have important implica- tions both for comparisons of modeled atmospheric carbon dioxide concentrations to observations and for carbon dioxide inversion studies, which use estimates of atmospheric transport of carbon dioxide in conjunction with measurements of atmospheric carbon dioxide concentrations to infer the spatio-temporal distribution of surface carbon dioxide fluxes. Furthermore, use of the complete Exner function equation affects the vertical velocity and water mixing ratio fields, causing significant changes in accumulated precipitation over the region.
TL;DR: In this paper, the authors used the Regional Atmospheric Modeling System (RAM) version 4.4 to simulate an extreme heavy rainfall event in the mountainous provinces of central Vietnam, resulting in severe flooding along local rivers.
Abstract: From 24 to 26 November 2004, an extreme heavy rainfall event occurred in the mountainous provinces of central Vietnam, resulting in severe flooding along local rivers. The Regional Atmospheric Modeling System, version 4.4, is used to simulate this event. In the present study, the convective parameterization scheme includes the original Kain–Fritsch scheme and a modified one in which a new diagnostic equation to compute updraft velocity, closure assumption, and trigger function are developed. These modifications take the vertical gradient of the Exner function perturbation into account, with an on–off coefficient to account for the role of the advective terms. According to the event simulations, the simulated precipitation shows that the modified scheme with the new trigger function gives much better results than the original one. Moreover, the interaction between convection and the larger-scale environment is much stronger near the midtroposphere where the return flow associated with lower-level ...
TL;DR: Alternative forms of the vertical momentum equation that use the Exner function, instead of pressure, in the pressure gradient term are found to lead to more accurate representations of the normal mode frequencies for the schemes having good conservation properties.
TL;DR: In this paper, an acoustic wave equation for the perturbation Exner function P9 is used to diagnose sources of infrasound in anumerical simulation of a convective storm.
Abstract: Thispaperpresentsaconvenientmethodfordiagnosingthesourcesofinfrasoundin anumericalsimulation of a convective storm. The method is based on an exact acoustic wave equation for the perturbation Exner function P9. One notable source term (Suu) in the P9 equation is commonly associated with adiabatic vortex fluctuations, whereas another (Sm) is directly connected to the heat and mass generated or removed during phase transitions of moisture. Scale estimates suggest that other potential sources are usually unimportant. Simplenumericalsimulationsofadisturbedvortexandevaporatingclouddropletsarecarriedouttoillustrate the infrasound of Suu and Sm. Moreover, the diagnostic method is applied to a towering cumulonimbus simulationthat incorporatesmultiplecategories of ice, liquid, and mixed-phase hydrometeors.The sensitivity of Sm to the modeling of the hail-to-rain category conversion is briefly addressed.