The improved parameterization of unresolved features of tropical convection is a central challenge in current computer models for long-range ensemble forecasting of weather and short-term climate change. Observations, theory, and detailed smaller-scale numerical simulations suggest that convective momentum transport (CMT) from the unresolved scales to the resolved scales is one of the major deficiencies in contemporary computer models. Here, a combination of mathematical and physical reasoning is utilized to build simple stochastic models that capture the significant intermittent upscale transports of CMT on the large scales due to organized unresolved convection from squall lines. Properties of the stochastic model for CMT are developed below in a test column model environment for the large-scale variables. The effects of CMT from the stochastic model on a large-scale convectively coupled wave in an idealized setting are presented below as a nontrivial test problem. Here, the upscale transports from stochastic effects are significant and even generate a large-scale mean flow which can interact with the convectively coupled wave.atmospheric convection parameterization | tropical atmospheric convection M oist convection in the tropics has a profound impact on the ability to predict extended-range weather and short-term climate change (1). The reason for this is the observed complex multiscale features of organized, coherent, tropical convection across a wide range of scales varying from tens of kilometers and a few hours to the planetary scale of the order of 40,000 km on intraseasonal timescales with significant energy transfer across these scales (2-5). The current computer models for prediction of both weather and climate involve general circulation models (GCMs) where the physical equations for these extremely complex flows are discretized in space and time and the effects of unresolved processes are parameterized according to various recipes. Typical mesh spacings of the order of 40-80 km are used for extended-range ensemble predictions and of the order of 100-200 km for climate simulations; despite a large effort and some advances, the skill of contemporary GCMs in capturing these large-scale patterns in the tropics is modest in the best circumstances (6). Contemporary observations (7-9), theory (10-13), and cloud-resolving numerical simulations (14, 15) all point to the role of convective momentum transport (CMT) as one of the main mechanisms where organized moist convection on smaller scales affects the wave patterns on larger scales; the dynamic effects of CMT are poorly resolved by contemporary GCMs (16), although recent deterministic parameterization has improved the mean climatology (17, 18) and the El Niño Southern Oscillation (19). The main goal of this contribution is to develop a simple stochastic model to capture unresolved features of CMT.The motivation for such a stochastic model comes from the observations of CMT (7,8); these detailed observations show that, in the mean, CMT is downscale (damp...