Updraft and Downdraft Core Size and Intensity as Revealed by Radar Wind Profilers: MCS Observations and Idealized Model Comparisons

Author:

Wang Dié1ORCID,Giangrande Scott E.1ORCID,Feng Zhe2ORCID,Hardin Joseph C.2ORCID,Prein Andreas F.3ORCID

Affiliation:

1. Environmental and Climate Sciences Department Brookhaven National Laboratory Upton NY USA

2. Pacific Northwest National Laboratory Richland WA USA

3. National Center for Atmospheric Research Boulder CO USA

Funder

U.S. Department of Energy

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Reference73 articles.

1. ARM(2014).Laser disdrometer (PARS2). 2014‐01‐01 to 2015‐11‐30 Arm Mobile Facility (MAO) Manacapuru Amazonas Brazil; AMF1 (m1); 2012‐01‐01 to 2016‐12‐31 Southern Great Plains (SGP) central facility Lamont OK (C1). ARM Data Center . Retrieved fromhttp://doi.org/10.5439/1150252(Compiled by M. Bartholomew Y. Shi and D. Wang. Data set accessed 2019‐01‐20.)https://doi.org/10.5439/1150252

2. Balloon‐Borne Sounding System (SONDEWNPN). 2014‐01‐01 to 2015‐11‐30, Arm Mobile Facility (MAO) Manacapuru, Amazonas, Brazil; AMF1 (m1); 2012‐01‐01 to 2016‐12‐31, Southern Great Plains (SGP) central facility, Lamont, OK (C1).;ARM;ARM Data Center,2019

3. Characteristics of Strong Updrafts in Precipitation Systems over the Central Tropical Pacific Ocean and in the Amazon

4. Sensitivity of a Simulated Squall Line to Horizontal Resolution and Parameterization of Microphysics

5. Resolution Requirements for the Simulation of Deep Moist Convection

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