PPT-Satellite and Aircraft Observations of Upper-Level Outflow

Hurricanes Iselle and Julio 2014 Julie K Stapleton Anthony L Borrego Sara C Reynolds Elizabeth R Sanabia and Bradford SBarret t Oceanography Department US Naval Academy Annapolis M. GloPac. campaigns. Karen Rosenlof. 1. and Eric Ray. 2. 1. NOAA ESRL CSD. 2. CIRES, University of Colorado. Boulder, CO. HIAPER Pole-to-Pole Observations (HIPPO. ) . What is HIPPO?. High resolutions measurements over the entire latitude range of the Pacific. Dr. . DaNa. L. . Carlis. NOAA/NWS/NCEP/EMC. September 13, 2011. Significant contributions from Brad . Ballish. (NCO), . Ron . Gelaro. (GMAO), Stan Benjamin (ESRL), Jim Jung (JCSDA), Dennis Keyser (EMC), . Randall Martin. with . contributions from. Shailesh. . Kharol. , . Gray . O’Byrne, . Akhila. . Padmanabhan. , . Aaron van . Donkelaar. . 2013 China Emissions . Workshop, Beijing. 28 June 2013. Lok. models: Examples. ATM 569. Fovell. Fall . 2015. (See course notes, Chapter 16). 1. Integrating the . adjoint. 2. (1) Run the control model to time . N. and save . C. n. every time step. (2) Initialize . Ellen Howell (Arecibo Observatory) and Amy Lovell (Agnes Scott College). Hyakutake. Comets: where do they come from?. Icy bodies ejected during giant planet formation. Remnants of early solar system. Pacific Northwest Weather Workshop. 4th March 2016. NOAA Western Regional Center, Seattle, WA. Funded by . NASA grants NNX13AG71G, NNX15AL38G, and NNX16AD75G . and . NSF grant AGS-1503155. . From Synoptic to Microscale: . for Space Launch Operations. Douglas G. Thorpe*. Space Propulsion Synergy Team & Co-founder of . the. USA. party.com. ; Mt. Sterling, KY. Daric Escher‡. LibertyWorks. Rolls-Royce, Indianapolis, IN 46225-1103. . Tianfeng Chai. 1,2,3. , . Hyuncheol. Kim. 1,2,3. , and Ariel Stein. 1. 1: NOAA/OAR/Air Resources Laboratory (ARL). 2: Cooperative Institute for Climate & Satellites-Maryland (CICS-MD). 3: University of Maryland, College Park, MD. Sub-Orbital Passenger Aircraft for Space Launch Operations Douglas G. Thorpe* Space Propulsion Synergy Team & Co-founder of the USA party.com ; Mt. Sterling, KY Daric Escher‡ LibertyWorks Rolls-Royce, Indianapolis, IN 46225-1103 mesoscale. convective systems. Thomas Kilpatrick. 1,2. , Shang-Ping Xie. 1,2. 1. Scripps Institution of Oceanography, La Jolla, CA.. 2. International Pacific Research Center, Honolulu, HI.. Introduction. the Indonesia 2015 peat fire season case study. Antonio G. Bruno. 1,2. , Jeremy J. Harrison. 1,2. , David P. Moore. 1,2. , Martyn P. Chipperfield. 3,4. , and Richard . J. Pope. 3,4. 1. University of Leicester, School of Physics and Astronomy, Leicester, UK (. ATM 562. Fovell. Fall 2021. (See course notes, Chapter 17). 1. Recap of theory. 2. Background: integrate model. Initial condition is . u. 0. . Integrate for . N. time steps.. We can relate the . final forecast. Background:. In the past two decades, improved measurements of acceleration due to gravity have allowed for accurate detection of temporal gravity change. Terrestrial gravimeters can sense changes of gravity induced by elevation or mass changes, including local effects that may bias regional studies. Satellite instrumentation can detect large scale mass changes on a regular basis. The minimum resolution of the GRACE satellite is about 400 km, which is too large for the size of most, direct regional studies. Also, satellites are limited by their life of deployment. Both techniques can be scaled to (in)validate change models generated from other geophysical observations including water storage (underground and glacial), geoid definition, isostatic adjustments and tectonic activity. . 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).