PPT-Clouds and Aerosols IPCC AR5 – Chapter

7 Ashley Evanoski Cole amp Christina McCluskey ATS 786 12 October 2014 Clouds in Present Day Climate System First time cloud and aerosol has been in the same chapter in an IPCC report Improved observations of clouds resolving multilayer cloud systems. Candidate material. The following. collection of slides were assembled from various presentations and from the Afternoon Constellation Operations Coordination Plan.. As mentioned at the meeting, several of the slides are out-dated – they typically do not take into account later missions, i.e., OCO-2, GCOM-W1, or Glory.. Robert Wood. , Matthew . Wyant. , Christopher S. . Bretherton. , Jasmine . Rémillard. , . Pavlos. . Kollias. , Jennifer Fletcher, Jayson . Stemmler. ,. . S. . deSzoeke. , Sandra . Yuter. , Matthew Miller, David . Robert Wood. University of Washington. W. ith contributions . from . Eowyn. Baughman, Dan . Grosvenor, Daniel McCoy, Chris . Terai. , Matt . Lebsock. , Dave Leon, Jeff Snider, Tony . Clarke, . Duli. Presented by Lorraine A. Remer. NASA/Goddard Space Flight Center. Basis of remote sensing. Remote sensing of clouds and aerosols. Observations of aerosol modification of cloud microphysics. 3.1 Explanation. The SOCRATES Planning . Team. : . Greg . McFarquhar. (. mcfarq@atmos.uiuc.edu. ),. Roj. . Marchand. , . Robert . Wood, Chris . Bretherton. , Alain . Protat. , Patricia Quinn, Steven . Siems. , Simon Alexander, and Bob Weller. Aerosol-Cloud-Climate Interactions. . Spring Quarter 2015. Logistics. Class . webpage. . Class meets 1:30-2:50 Mondays and Wednesdays in Room 406, ATG Building. Instructor: . Typical cold sea surface temperatures, in conjunction with the subsidence associated with the subtropical high, are responsible for the formation of a shallow cool moist marine boundary layer capped by a strong inversion. Marine stratus clouds form in this marine boundary layer. . Jessie Creamean. Andrew Martin. Thursday. , . January 22, 2015. Current Conditions I. High AOD plumes (Jan21a and Jan21b) are in dry slot of mature in N. Central Pac. These likely correspond to plumes Jan20a and Jan20b, respectively.. of. aerosols over clouds . and. clear skies determined using CALIPSO . and. the A-Train. Robert Wood. , . Duli. . Chand. , Tad Anderson. University of Washington. VOCALS RF04, 21 November 2008. Effect of aerosol layer on TOA SW radiation. . Spring Quarter 2015. Logistics. Class . webpage. . Class meets 1:30-2:50 Mondays and Wednesdays in Room 406, ATG Building. Instructor: . Prof. . Robert . Wood . [ATG . 718, Phone . Sara Purdue and . Haviland. . Forrister. 1. Introduction. Direct effects: biomass burning aerosols absorb light (BC and . BrC. ) and scatter light (OA, sulfate). Semi-direct effects: heating effects of aerosols in and around clouds. Director, Southern Regional Climate Center. IPCC AR6 WG1. Near-final draft released in August 2021. Addresses how the climate has changed and may/will change. Doesn’t consider impacts (WG2) or mitigation (WG3). Elisabeth Andrews. CATCOS Workshop, June 2016. What is climate?. Climate is the average weather. The standard averaging time for climate is 30 years. “Weather is what you’re wearing, climate is what’s in your closet”. the Characterization of Clouds, Aerosols and the . Cryosphere. in Climate . Models. Parameterization development. How have changing forcing agents influenced sea ice over the last few decades?. How do improvements to process level representation influence our interpretation of that climate change?.