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

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 . 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. Liu et al. 2010. Review By: . Gus . Alaka. and Doug . Stolz. 20 February 2014. ATS 780. Background. C. T. R. Wilson’s Hypotheses: . Thunderstorms . AND. electrified shower clouds are the “batteries” of the global DC electrical circuit. Adopted (with permission) and later tested by F. Whipple.. precipitation variability over the Gulf Stream and . the Kuroshio. Shoshiro Minobe . and Shogo . Takabeyashi. (Hokkaido University, Sapporo, Japan) . Outline. . Introduction. . Global View. . Gulf Stream . Kaustav. . Chakravarty. Richard H. Johnson. Paul E. . Ciesielski. Colorado State University. J. L. Davison. University of Louisville. Third Symposium on Prediction of the Madden-Julian Oscillation: Processes, Prediction and . 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?. Water Cycle (Pete R. and Andrea). Energy Budget. Implied Ocean Heat Transport (. Yury. /Andrea). MERRA-2 Water and Energy. Diurnal Precipitation – MERRA-2. Contributed by Winston Chao. Diurnal Precipitation: TRMM. Observations. Brian A. Colle. 1. . and Aaron Naeger. 2. 1. School . of Marine and Atmospheric Sciences, Stony Brook University, Stony . Brook, NY. 2. University of Alabama at Huntsville. This work is supported by NASA PMM #. Objective:. LUMIP aims to advance understanding of the impacts of land-use and land-cover change (LULCC) on climate, addressing the following questions:. (1) What are the effects of LULCC on climate and biogeochemical cycling?. 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) . Claire . Bulgin. University. of Reading, National Centre for . Earth. Observation. Background. Every measurement we make (both in-situ or remotely sensed) deviates from the ‘true’ surface temperature due imperfections in the instrumentation and measurement process. Therefore, in order to use the data correctly, you must consider the uncertainty in the measurement.. 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.