An Analysis of the Importance of a Fully-Coupled Atmosphere and Land-Surface When Considering the Impact of Multi-Scale Land Spatial Heterogeneity on Cloud Development

Jason Simon,Finley Hay-Chapman,Andrew Bragg,Tyler Waterman,Paul Dirmeyer,Nathaniel Chaney

doi:10.5194/egusphere-egu21-13379

Abstract

&lt;p&gt;&lt;span&gt;Land-surface heterogeneity is known to play an important role in land-surface hydrology, which drives the bottom boundary condition for atmospheric models in numerical weather prediction (NWP) applications. However, the ultimate impact of land-surface heterogeneity on atmospheric boundary layer (ABL) development is still an open problem with implications for sub-grid scale (SGS) parameterizations for both NWP and climate modeling. Large-eddy simulation (LES) is often used to study the effects of land-surface heterogeneity on ABL development, most typically via specified surface fields which are not influenced by the atmosphere (i.e. semi-coupled). Heterogeneous land surfaces have been seen in previous studies to have a significant influence on ABL dynamics, particularly cloud production, in certain cases when semi-coupled to the atmosphere. &lt;/span&gt;&lt;/p&gt;&lt;p&gt;&lt;span&gt;Here we use the Weather Research and Forecasting (WRF) model as an LES with both semi-coupled and fully-coupled land surfaces to investigate the impact of two-way coupling on the interaction between heterogeneous land surfaces and daytime ABLs. For semi-coupled simulations, the HydroBlocks land-surface model is run offline, drive&lt;/span&gt;&lt;span&gt;n by 4-km NLDAS-2 meteorology with Stage-IV radar rainfall data, and then used to specify the bottom boundary in WRF. The WRF-Hydro model is used for cases where the land surface is fully coupled to the WRF model. Both land-surface models use the Noah-MP model as their underlying physics package and add both subsurface and overland flow routing. &lt;/span&gt;&lt;span&gt;The WRF model uses a 100-m horizontal resolution, and the land-surface models use &lt;/span&gt;&lt;span&gt;high resolution (30 m) datasets that were upscaled to match the LES resolution for elevation, landcover, and soil type using NED, NLCD, and POLARIS respectively. &lt;/span&gt;&lt;span&gt;These LES experiments are performed over the ARM Southern Great Plains Site&lt;/span&gt;&lt;span&gt; atmospheric observatory in Oklahoma during the Summer of 2017 with a grid size of 100 km x 100 km to imitate a single cell in a modern climate model. &lt;/span&gt;&lt;span&gt;The impact of land-surface heterogeneity on the atmosphere is evaluated by comparing simulations using the fully heterogeneous land surfaces with simulations where the land surface is homogenized at each timestep, taking a domain-wide spatial mean value at every grid cell. &lt;/span&gt;&lt;span&gt;Results are evaluated primarily by the differences in the development of clouds and evolution of turbulent kinetic energy in the ABL. &lt;/span&gt;&lt;/p&gt;

Full Text