Presenter: jacob.shpund (Unlicensed)
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Overall, the P3 microphysics shows a comparable climatology to MG2. P3 improves both the cloud shortwave and longwave radiative forcing in the Northern Hemisphere and the high cloud fraction in the Tropics. The ice water path is increased with P3 compared with MG2, and the frequency of heavy precipitation rates over the continental US is larger with P3 and more consistent with observations. There are specific areas needed further improvements such as relatively low liquid water content at midlatitudes, and low-cloud fractions over the Southern Hemisphere.
Date
04
Time
- PT: 8:30 am
- ET: 11:30 am
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Attendees
- Luke Van Roekel
- jacob.shpund (Unlicensed)
- Jiwen Fan (Unlicensed)
- Ruby Leung
- Jim Benedict
- Darin Comeau
- Jon Wolfe
- Jayesh Krishna
- Matt Turner (Unlicensed)
- Matt Hoffman
- Chris Golaz
- Sha Feng
- Qing Li (Unlicensed)
- Qi Tang
- Steven Brus
- Stephen Price
- Trevor Hillebrand
- Nicole Jeffery
- Teklu Tesfa
- Carolyn Begeman
- Katherine Smith
- Oksana Guba
- Bryce Harrop
- Chris Terai
- Marcus van Lier-Walqui (Unlicensed)
- Shaocheng Xie
- Andy Salinger
- Mingxuan Wu
- Peter Caldwell
- Yilin Fang
- Peter Bogenschutz
- Hyun-Gyu Kang
- David C. Bader
- Steve Klein
- Peter Schwartz
- Xiaohong Liu (Unlicensed)
- Yan Feng
- Mikhail Ovchinnikov
- Mathew Maltrud
- Ryan Forsyth
- Nicole Jeffery
- Amrapalli Garanaik (Unlicensed)
- Teklu Tesfa
- Katherine Smith
- Xubin Zeng
- Mark Taylor
- Susannah Burrows
- Trevor Hillebrand
- Qi Tang
- Xujing Jia Davis
- Phil Rasch
- Shixuan Zhang
- Karthik Balaguru
Presentation
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