ARM high-resolution observations of air motion are coupled with global satellite data to understand differences in drizzle and rain formation in clouds that form over land and ocean. The insights should help improve future model simulations of rain formation.
Warm liquid clouds are of fundamental importance to the global climate since their particle-growth processes (the growth of droplets from cloud particles to drizzle to rain) play a key role in the hydrological cycle of the Earth. Lack of a full understanding of these particle-growth processes and how to best represent them in Earth system models is a source of uncertainty in future climate projections. Previous studies have indicated differences in particle growth processes and in the transition from cloud to drizzle in clouds that form over land and ocean. This study combines satellite observations with detailed ARM ground-based observations to explore the hypothesis that these differences between clouds over land and ocean are caused by different intensities of rising air motion (convective updrafts) in the clouds.
This study shows that a stronger updraft increases the height at which significant droplet coalescence begins, and also prolongs the lifetime of falling drops, which promotes larger droplet growth. These results point to the critical role of the strength of the convective updraft in the warm-rain formation process. These processes occur at cloud-scales smaller than the grid boxes of most weather and Earth system models, so their effects must be represented by numerical formulations known as ‘parameterizations’. This study indicates important paths to improving these parameterizations, and hence future simulations of global rainfall, in Earth system models.
This study provides new insight into the role of vertical velocity in the warm-rain formation process using both NASA satellite observations and surface observations obtained from a U.S. Department of Energy (DOE) ARM mobile observing system that operated in the Azores. Results from the satellite data, from the ARM surface dataset, and from a one-dimensional model all produce a consistent result, that the land-ocean differences in the warm-rain formation process can be (at least partly) explained by the land-ocean differences in the intensity of cloud updraft when the aerosol effects are minimized. The present result is important because it is the first clear evidence of cloud motion affecting the cloud-precipitation process in warm clouds. Current global climate models (GCMs) cannot resolve these cloud-scale motions which we show are important in simulating realistic warm-rain clouds.
This article provides the first detailed analysis of the land-ocean difference in warm-rain clouds using the contoured frequency by optical depth (CFOD) method. And for the first time, the role of updraft intensity in the warm-rain formation process has been demonstrated by minimizing aerosol effects; namely, that updraft intensity affects both the height at which significant coalescence begins and the lifetime of falling drops. This study encourages focusing on other important variables such as vertical velocity beside aerosol effects in warm-rain clouds, which represents a new way of understanding the warm-rain formation process that can contribute to climate model improvement in representing warm-rain clouds.
ARM Program Manager
Joint Institute for Regional Earth System Science and Engineering, UCLA
Jet Propulsion Laboratory, California Institute of Technology
This study was carried out at Jet Propulsion Laboratory, California Institute of Technology under a contract with NASA. This study was supported by NASA Grants NNN13D455T. K. Suzuki was supported by NOAA’s Climate Program Office’s Modeling, Analysis, Predictions, and Projections Programme with the grant number NA15OAR4310153, JAXA/EarthCARE and JAXA/GCOM-C projects. Data were obtained from the Atmospheric Radiation Measurement (ARM) Program sponsored by the US Department of Energy, Office of Science, Office of Biological and Environmental Research.
Takahashi H., K. Suzuki, and G. Stephens. 2017. "Land-Ocean Differences in the Warm-Rain Formation Process in Satellite and Ground-Based Observations and Model Simulations," Quarterly Journal of the Royal Meteorological Society, 143(705), 1804-1815. DOI: 10.1002/qj.3042.
SC-23.1 Climate and Environmental Sciences Division, BER
BER supports basic research and scientific user facilities to advance DOE missions in energy and environment. More about BER
May 10, 2019
Quantifying Decision Uncertainty in Water Management via a Coupled Agent-Based Model
Considering risk perception can improve the representation of human decision-making processes in age [more...]
May 09, 2019
Projecting Global Urban Area Growth Through 2100 Based on Historical Time Series Data and Future Scenarios
Study provides country-specific urban area growth models and the first dataset on country-level urba [more...]
May 05, 2019
Calibrating Building Energy Demand Models to Refine Long-Term Energy Planning
A new, flexible calibration approach improved model accuracy in capturing year-to-year changes in bu [more...]
May 03, 2019
Calibration and Uncertainty Analysis of Demeter for Better Downscaling of Global Land Use and Land Cover Projections
Researchers improved the Demeter model’s performance by calibrating key parameters and establi [more...]
Apr 22, 2019
Representation of U.S. Warm Temperature Extremes in Global Climate Model Ensembles
Representation of warm temperature events varies considerably among global climate models, which has [more...]
List all highlights (possible long download time)