Abstract

We develop a new approach that resolves cloud area distributions of single-layer shallow cumuli from ground-based observations. Our simple and computationally inexpensive approach uses images obtained from a Total Sky Imager (TSI) and complementary information on cloud base height provided by lidar measurements to estimate cloud equivalent diameter (CED) over a wide range of cloud sizes (about 0.01–3.5 km) with high temporal resolution (30 s). We illustrate the feasibility of our approach by comparing the estimated CEDs with those derived from collocated and coincident high-resolution (0.03 km) Landsat cloud masks with different spatial and temporal patterns of cloud cover collected over the Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) site. We demonstrate that (1) good (~7%) agreement between TSI and Landsat characteristic cloud size can be obtained for clouds that fall within the region of the sky observable by the TSI and (2) large clouds that extend beyond this region are responsible for noticeable (~16%) underestimation of the TSI characteristic cloud size. Our approach provides a previously unavailable dataset for process studies in the convective boundary layer and evaluation of shallow cumuli in cloud-resolving models.

Highlights

  • Shallow cumuli are observed frequently over many continental and marine regions of the world.They consist mainly of small (

  • Our approach is computationally inexpensive and relies on sky images obtained from Total Sky Imager (TSI) and complementary information on cloud base height provided by lidar measurements

  • We illustrate performance of our approach using coincident 0.03-km Landsat cloud masks obtained for five periods with single-layer shallow cumuli over the Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP)

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Summary

Introduction

Shallow cumuli are observed frequently over many continental and marine regions of the world. Since cumuli areoftypically small (

Approach
Interpolation over Image Obstructions
Projection of Cloud Mask from Hemispherical to Planar Coordinate System
Computation of Cloud Areas and the Corresponding CED
Landsat
Results
Conclusions
14 June 2017
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