PPT-MERRA-2 Cloud Radiative

Author : delcy | Published Date : 2023-10-04

Forcing Validation Peter Norris MERRA2 Rollout NASAGSFC June 4 2015 Introduction Compare MERRA2 TOA cloud radiative forcing against CERES EBAF and MERRA All

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MERRA-2 Cloud Radiative: Transcript


Forcing Validation Peter Norris MERRA2 Rollout NASAGSFC June 4 2015 Introduction Compare MERRA2 TOA cloud radiative forcing against CERES EBAF and MERRA All results use monthly means aggregated into 14 year averages for the period Mar 2000 . R adiative - , Page 1 Radiative and Radiative - Convecti ve Equilibrium Introduction The energy balance of the Earth’ ytem i quite intricate with numerou Astrophysical and Laboratory Plasmas. Lecture 1: Temperature-Density regime. . Many physical processes. . Focus on . Atomic+Plasma. interactions. . Atomic properties are . intrinsic. , . independent of external factors (temp, den, etc.). tropical cyclones. Robert Fovell and . Yizhe. Peggy Bu. University of California, Los Angeles. rfovell@ucla.edu. 1. Thanks to. : . Greg . Thompson, NCAR/. DTC; Ligia . Bernardet. and Mrinal . Biswas. Corrections. Peter Schnatz. Stony Brook University. Radiative. Events. In scattering experiments, a photon may be emitted by a charged particle due to . Bremsstrahlung. radiation.. This type of radiation is due to the deceleration of a charged particle as it approaches the . by . means of MBE method. Ashida. . lab. M1 . K. amizono Kenta. Introduction. All-optical switching devices. Excitons . and light in the high-quality system . Background . Previous results. Temperature dependence of DFWM spectrum. In astronomy, the main source of information about celestial bodies and other objects is the visible light or more generally electromagnetic radiation.. From Wikipedia.. It also is important for the atmosphere of Earth, so you’ll meet it if you are going into Earth atmosphere science…. the . Radiative Effects . of . Black Carbon Internal Mixing. Charles Li. Group Meeting Presentation. October 1, 2014. Group Meeting 10/1/14. 1. Black Carbon (BC) Direct Radiative Forcing:. +0.71 W m. of the MERRA-2 Assimilated Ozone Product. Gordon . Labow. Krzysztof . Wargan. Stacey . Frith. Steven Pawson. Gary . Partyka. September, 8, 2016. What is MERRA-2?. MODERN-ERA RETROSPECTIVE . ANALYSIS . radiative. forcing. Heald. et al. 2013 ACPD. Ashley Pierce. Aerosol seminar, February 24th. 1. outline. Aerosols and climate change. IPCC on aerosols. Direct . Radiative . Effect vs. . Direct Radiative . 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. 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. Xiaoming Hu. 1. , Sergio A. Sejas. 2. , Ming Cai. 3. , . Zhenning. Li. 4. and Song Yang. 1. 1. School of Atmospheric Sciences, Sun . Yat-sen. University, Guangzhou, China. 2. NASA Langley Research Center, Climate Science Branch, Hampton, Virginia, USA. Kerry Emanuel. Massachusetts Institute of Technology. Several Possibly Inter-related Enigmas of the Tropical Atmosphere. Why does moist convection often cluster?. What determines the number of tropical cyclones on the planet?. Natural Environments . Day-of-Launch Working Group Meeting Fall 2023. Patrick White (patrick.w.white@nasa.gov) - Earth-GRAM Lead. MSFC / Natural Environments Branch. Outline. Goals. Overview. Current Global Reference Atmospheric Model (GRAM) Suite Planned Updates to Earth-GRAM.

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