PPT-Evaluating the Diurnal and Semidiurnal Cycle of Precipitation in CMIP6 Models Using Satellite-

Author : beatrice | Published Date : 2022-06-11

Tang S P Gleckler S Xie J Lee C Covey C Zhang MS Ahn 2021 Evaluating Diurnal and SemiDiurnal Cycle of Precipitation in CMIP6 Models Using Satellite and GroundBased

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Evaluating the Diurnal and Semidiurnal Cycle of Precipitation in CMIP6 Models Using Satellite-: Transcript

Tang S P Gleckler S Xie J Lee C Covey C Zhang MS Ahn 2021 Evaluating Diurnal and SemiDiurnal Cycle of Precipitation in CMIP6 Models Using Satellite and GroundBased Observations . in . Near. -Surface Salinity. Kyla Drushka. 1. , . Sarah . Gille. 2. , Janet . Sprintall. 2. . kdrushka. @. apl.uw.edu. 1. Applied . Physics Lab, Univ. of . Washington . 2. Scripps Inst. of Oceanography. of . Salinity. Kyla Drushka. 1. , . Sarah Gille. 2. , Janet Sprintall. 2. . kdrushka@apl.uw.edu. 1. Applied Physics Lab, Univ. of Washington . 2. Scripps Inst. of Oceanography. Aquarius Science Team Meeting. Carl Mears. Remote Sensing Systems. Why do we care about . the diurnal cycle?. Most polar orbiting satellites drift in local measurement time – need estimate of diurnal cycle to adjust for this.. Model validation studies. precipitation variability over the Gulf Stream and . the Kuroshio. Shoshiro Minobe . and Shogo . Takabeyashi. (Hokkaido University, Sapporo, Japan) . Outline. . Introduction. . Global View. . Gulf Stream . Richard H. Johnson. Colorado State University. T. . Ushiyama. (Andy . Newman , Brian . McNoldy. , and Paul . Ciesielski. ). MAHASRI/. HyARC. workshop, 5-7 March 2009, . DaNang. , Vietnam . Why do we care about the diurnal cycle?. in Hainan Island. Lei Zhu. Paul . Markowski. , . Zhiyong. . Meng. and . Fuqing. Zhang. Research purpose. T. ry to understand the climatology . of . diurnal. . precipitation cycle in Hainan Island. the Impact of Islands on the Tropical Climate. Timothy W. . Cronin*, Kerry A. Emanuel. Program in Atmospheres, Oceans, and Climate, Massachusetts . Institute of . Technology. 77 . Massachusetts Avenue, Cambridge . Luke Oman. luke.d.oman@nasa.gov. SAGE III/ISS STM – Oct. 30, 2019 . 1. Luke Oman. 1. , Sarah Strode. 1,2. , . Ghassan Taha. 1,2. , and Mark Schoeberl. 3. 1. NASA/GSFC, Greenbelt, MD, USA. 2. University Space Research Association, Columbia, MD, USA. of the UM in different parts of the world.. Humphrey Lean, Kirsty Hanley, Stuart Webster, Will Keat, Thorwald Stein, Todd Lane, Martin Jucker, Elizabeth Kendon and Giorgia Fosser. Met Office has run 1.5km UK version of Unified Model for about 10 years (UKV). . over Sumatra Island, Indonesia, on. synoptic disturbances and its relation to. the Madden-Julian Oscillation. Ayako SEIKI, Satoru YOKOI, and Masaki KATSUMATA. (JAMSTEC, Japan). Seiki et al. (2021), JMSJ. Olaf Morgenstern, NIWA, Wellington, New Zealand. 1. Introduction. The SAM is influenced by ozone depletion and increasing greenhouse gases. Using a regression analysis and sensitivity simulations, I assess the impacts of changes in these . Shuaiqi Tang. Pacific Northwest National Laboratory, Richland, WA, USA. 6/18/2022. Collaborators: Shaocheng Xie, Cheng Tao, Hsi-Yen Ma, and many others. Outline. Common issues in simulating diurnal cycle of precipitation (DCP) . Use NOAA Unique Combined Atmospheric Processing System (NUCAPS) Satellite Soundings to observe the tropical cyclone (TC) diurnal cycle. infrared (IR) and microwave (MW) soundings. Three case studies: Hurricanes Dorian (2019), Florence (2018), Irma (2017). x. . and NO. x. emissions over North America. . Daniel Jacob, Viral Shah, . Ruijung. Dang, Laura Yang. Shah et al., in prep.; Dang et al., in prep.. Lowest 2 km contributes only 30% of tropospheric NO.

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