Search Results
between humidity/temperature and heating/moistening, or likewise by automatic differentiation of nonlinear regression models ( Brenowitz and Bretherton 2019 ). Visualizing the LRF as a matrix does not predict the consequences of coupling the scheme to atmospheric fluid mechanics (i.e., the GCM’s “dynamical core”). Kuang (2010) takes this additional step by coupling CRM-derived LRFs with linearized gravity wave dynamics and further developing a vertically truncated ordinary differential equation
between humidity/temperature and heating/moistening, or likewise by automatic differentiation of nonlinear regression models ( Brenowitz and Bretherton 2019 ). Visualizing the LRF as a matrix does not predict the consequences of coupling the scheme to atmospheric fluid mechanics (i.e., the GCM’s “dynamical core”). Kuang (2010) takes this additional step by coupling CRM-derived LRFs with linearized gravity wave dynamics and further developing a vertically truncated ordinary differential equation
