Abstract
Abstract. Understanding the differences between regional simulations of land–atmosphere interactions and near-surface conditions is crucial for a more reliable representation of past and future climate. Here, we explore the effect of changes in the model's horizontal resolution on the simulated energy balance at the surface and near-surface conditions using the Weather Research and Forecasting (WRF) model. To this aim, an ensemble of 12 simulations using three different horizontal resolutions (25, 50 and 100 km) and four different land surface model (LSM) configurations over North America from 1980 to 2013 is developed. Our results show that finer resolutions lead to higher surface net shortwave radiation and maximum temperatures at mid and high latitudes. At low latitudes over coastal areas, an increase in resolution leads to lower values of sensible heat flux and higher values of latent heat flux, as well as lower values of surface temperatures and higher values of precipitation, and soil moisture in summer. The use of finer resolutions leads then to an increase in summer values of latent heat flux and convective and non-convective precipitation and soil moisture at low latitudes. The effect of the LSM choice is larger than the effect of horizontal resolution on the near-surface temperature conditions. By contrast, the effect of the LSM choice on the simulation of precipitation is weaker than the effect of horizontal resolution, showing larger differences among LSM simulations in summer and over regions with high latent heat flux. Comparison between observations and the simulation of daily maximum and minimum temperatures and accumulated precipitation indicates that the CLM4 LSM yields the lowest biases in maximum and minimum mean temperatures but the highest biases in extreme temperatures. Increasing horizontal resolution leads to larger biases in accumulated precipitation over all regions particularly in summer. The reasons behind this are related to the partition between convective and non-convective precipitation, specially noticeable over western USA.
Highlights
Most assessments of climate change impacts on ecosystems and societies are based on projections 25 performed by Regional Climate Models (RCMs) and/or Earth System Models (ESMs, IPCC, 2013; Arneth, 2019)
Over North America, our results indicate that the Weather Research and Forecast5 ing (WRF) simulation of temperature conditions using the CLM4 Land Surface Model (LSM) outperforms the simulation of mean maximum and minimum temperatures 435 generated by the NOAH and NOAH-MP LSMs, but it yields larger biases in extreme maximum and minimum temperatures (Figures 9 and 10)
This study has shown the effect of changes in horizontal resolution and LSM choice on the simulation of energy fluxes at the surface and temperature and water conditions in the near-surface
Summary
Most assessments of climate change impacts on ecosystems and societies are based on projections 25 performed by Regional Climate Models (RCMs) and/or Earth System Models (ESMs, IPCC, 2013; Arneth, 2019). Exploring inter-model differences in present climate simulations is necessary to understand their contribution to the spread in future climate projections, and to better characterize or even reduce the uncertainty in the simulation of the response to a given scenario (Cubasch et al, 2013). Understanding inter-model differences is important for paleoclimatic studies re lying on regional climate model simulations to bridge the gap between the local character of proxy reconstructions and ESM global simulations (e.g. PALEOLINK, Gómez-Navarro et al, 2018). Land-atmosphere interactions have been studied in the evaluation of climate model simulations, applying several metrics to characterize surface energy fluxes and near-surface conditions (Koven et al, 2013; 40 Dirmeyer et al, 2013; Sippel et al, 2017; García-García et al, 2019)
Sign-in/Register to view highlights & summary Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
