PPT-Atmospheric Correction Algorithm

Atmospheric Correction Algorithm for the GOCI Jae Hyun Ahn JooHyung Ryu Young Jae Park YuHwan Ahn Im Sang Oh Korea Ocean Research amp Development Institute Seoul National University. with . climate variability and change . Seminar in Atmospheric Science, EESC G9910. Diagnosing ENSO from atmospheric composition (ozone measured from space). Ziemke. et al. ., 2010; . Oman et al. ., 2011. Naba. K . Mondal. Tata Institute of Fundamental Research. Mumbai 400005, India. Brief History. Atmospheric neutrino experiments study neutrinos produced by cosmic ray interactions in the atmosphere.. Curtis Seaman. CIRA/Colorado State University. 23 May 2014. Without Terrain Correction. Pay attention to Hawaii, on the right edge of the swath – the only terrain in the scene. . Using Terrain Corrected Lat/Lon. The atmosphere is evil. Clouds. Humidity. Gasses. Pollution/haze. Different sun angles. clouds. Block pretty much everything in the V-MIR.. Shadows.. Annoying as heck.. Only solution, radar data. humidity. Evaluation of moisture characteristics associated with heavy daily rainfall. Dependence on region/season. Progressing to hourly rain gauge data and additional precursor diagnostics (e.g. wet bulb & dew point temperature). for the GOCI. Jae Hyun . Ahn. *. Joo-Hyung. . Ryu. *. Young Jae Park*. Yu-Hwan . Ahn. *. Im. Sang Oh**. Korea Ocean Research & Development Institute. Seoul National University. I n d e x _. Introduction . and Climate (Chap 6). Atmospheric General Circulation. Also: Global or planetary circulation. . The general circulation (GC) of the atmosphere is the totality of motions that characterize the . large scale. Donna Tiberi, RN. Standards Interpretation . p: 312-202-8073 e: dtiberi@HFAP.org. 1. Objectives. Upon completion of this program, the participant will: . List . the requirements for . completing the Plan of Correction for approval. Jeff Forbes. Department of Aerospace Engineering Sciences, . University of Colorado, Boulder, CO. Brief history of the lunar atmospheric tide, and recent resurgence in interest. Characterizing lunar tidal forcing. Corrections. Atmospheric Effects on EMR. Kodiak Island, AK – Volcanic ash and clouds (MODIS image). Learning Objectives. What are the main ways that the atmosphere affects light traveling through it?. Eric . Vermote . et . al.. NASA . Goddard Space Flight Center Code . 619. Eric.f.vermote@nasa.gov.  .  . LCLUC Spring Meeting, April 12-14, Hilton, Rockville, MD. Home . page: . http://modis-sr.ltdri.org. Andrey . Vlasenko. , Armin Köhl, Detlef . Stammer. Institut für . Meerskunde. Universität Hamburg. Hamburg. TASK. Task 1.2.1 Identification of the atmospheric response to ocean surface state changes. Measuring atmospheric pressure at different altitudes above sea . level. How does atmospheric pressure vary?. Objective. The purpose of this activity is to study atmospheric pressure variations, as we reach higher . EARTH SURFACE. gravity. random. motion. Weight of all air molecules is propagated to surface by random motion of molecules. Random motion of molecules causes pressure to be applied in all directions.