Mind the gap – Part 1: Accurately locating warm marine boundary layer clouds and precipitation using spaceborne radars

<p>Ground-based radar observations show that, over the eastern North Atlantic, 50&thinsp;% of warm marine boundary layer (WMBL) hydrometeors occur below 1.2&thinsp;km and have reflectivities of &lt;&thinsp;<span class="inline-formula">−17</span>&thinsp...

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Bibliographic Details
Main Authors: K. Lamer, P. Kollias, A. Battaglia, S. Preval
Format: Article
Language:English
Published: Copernicus Publications 2020-05-01
Series:Atmospheric Measurement Techniques
Online Access:https://www.atmos-meas-tech.net/13/2363/2020/amt-13-2363-2020.pdf
Description
Summary:<p>Ground-based radar observations show that, over the eastern North Atlantic, 50&thinsp;% of warm marine boundary layer (WMBL) hydrometeors occur below 1.2&thinsp;km and have reflectivities of &lt;&thinsp;<span class="inline-formula">−17</span>&thinsp;dBZ, thus making their detection from space susceptible to the extent of surface clutter and radar sensitivity.</p> <p>Surface clutter limits the ability of the CloudSat cloud profiling radar (CPR) to observe the true cloud base in <span class="inline-formula">∼52</span>&thinsp;% of the cloudy columns it detects and true virga base in <span class="inline-formula">∼80</span>&thinsp;%, meaning the CloudSat CPR often provides an incomplete view of even the clouds it does detect. Using forward simulations, we determine that a 250&thinsp;m resolution radar would most accurately capture the boundaries of WMBL clouds and precipitation; that being said, because of sensitivity limitations, such a radar would suffer from cloud cover biases similar to those of the CloudSat CPR.</p> <p>Observations and forward simulations indicate that the CloudSat CPR fails to detect 29&thinsp;%–43&thinsp;% of the cloudy columns detected by ground-based sensors. Out of all configurations tested, the 7&thinsp;dB more sensitive EarthCARE CPR performs best (only missing 9.0&thinsp;% of cloudy columns) indicating that improving radar sensitivity is more important than decreasing the vertical extent of surface clutter for measuring cloud cover. However, because 50&thinsp;% of WMBL systems are thinner than 400&thinsp;m, they tend to be artificially stretched by long sensitive radar pulses, hence the EarthCARE CPR overestimation of cloud top height and hydrometeor fraction.</p> <p>Thus, it is recommended that the next generation of space-borne radars targeting WMBL science should operate interlaced pulse modes including both a highly sensitive long-pulse mode and a less sensitive but clutter-limiting short-pulse mode.</p>
ISSN:1867-1381
1867-8548