- satellite orbits. Further Reading: Chapter 04 of the text book. Outline. - satellite sensor measurements
|
|
- Jared Howard Garrett
- 5 years ago
- Views:
Transcription
1 (1 of 12) Further Reading: Chapter 04 of the text book Outline - satellite orbits - satellite sensor measurements - remote sensing of land, atmosphere and oceans
2 (2 of 12) Introduction Remote Sensing: Remote observations of electro-magnetic radiation arriving from the earth system with sensors onboard satellites, aircrafts, etc. Reflection and emission Land, Oceans, and Atmosphere Currently there are about 4000 satellites orbiting the earth; the US has about 1000 Not all of these are scientific Defense Communications Global Positioning System (GPS) Advantages Cheapest way to repeatedly view the entire Earth Digital data (easy to manipulate) Dis-advantages High initial cost ( million dollars to build and launch) High-tech
3 Geo-stationary Orbit (3 of 12) Geo-stationary: Orbits over the equator Goes through one orbit every 24 hours Hence, it rotates at the same speed as the earth and sits over the same spot the entire time Approximately 22,000 miles above earth Takes 5 satellites to cover the entire disk
4 (4 of 12) Geo-stationary Satellites: Example Geostationary System The objective of the geostationary operational environmental satellite (GOES) system is to maintain a continuous data stream from a two-goes system, primarily to support the National Weather Service requirements. The program objective is to meet requirements by procuring, through the GOES Acquisition Manager (NOAA/SAO) and NASA/GSFC, spacecraft, instruments, launch services, and ground equipment. The GOES program also invests in new product development and assists with implementing the approved products into operations.
5 (5 of 12) Polar Orbit Orbits over the poles Takes approximately 100 minutes to complete an orbit Can view the entire earth s surface in approximately 2-6 days Approximately 470 miles above the earth Also called Sun synchronous Example: Polar Orbiting NASA s Terra Platform Flying at an altitude of 705 km, Terra orbits the Earth once every 98 minutes in a near-polar orbit. The spacecraft descends southward across the equator at 10:30 a.m., when cloud cover is minimal and its view of the surface is least obstructed. As Terra orbits, notice that the Earth is also spinning, so that adjacent orbits are offset somewhat at the equator and there is a small gap between the MODIS instrument's viewing swaths. It will take a little more than 1 day for these gaps to be filled on subsequent overpasses, so that MODIS will provide us snapshots of the entire surface of the Earth within every 2 days.
6 (6 of 12) Remote Measurements Most satellite sensors measure radiation This radiation can either be sunlight reflected from some surface Land Atmosphere Oceans Can also measure (emitted) longwave radiation coming from the earth system Different sensors are designed to detect different types of radiation Images can be simple pictures, typically high resolution sensors -(Pentagon, San Francisco, Costa del Sol) Multi-spectral sensors measure reflected solar radiation at different wavelengths Moderate Resolution Imaging Spectroradiometer (MODIS) Multi-angle sensors measure reflected solar radiation at different directions Multi-angle Imaging Spectroradiometer (MISR)
7 (7 of 12) Remote Sensing of Land Deforestation: Amazon
8 (8 of 12) Remote Sensing of Land Mapping land covers from satellite data an example
9 (9 of 12) Remote Sensing of Land Monitoring global vegetation greenness from satellite data
10 (10 of 12) Remote Sensing of the Atmosphere Example atmospheric products from MODIS
11 (11 of 12) Remote Sensing of Oceans MODIS Sea Surface Temperature (SST) MODIS Ocean Color
12 (12 of 12) Remote Sensing of the Cryosphere 1999 seasonal sea ice concentrations in the Arctic and Antarctic at the approximate seasonal maximum and minimum. Images courtesy of the National Snow and Ice Data Center, University of Colorado.
SAN FRANCISCO STATE UNIVERSITY NAME DEPARTMENT OF GEOSCIENCES Spring 2013
SAN FRANCISCO STATE UNIVERSITY NAME DEPARTMENT OF GEOSCIENCES Spring 2013 METR 415/715: MONTEVERDI QUIZ 1 Open Book and Open Notes 200 points, 45 minutes 1. Compute the altitude of a geostationary orbit
More informationRemote Sensing I: Basics
Remote Sensing I: Basics Kelly M. Brunt Earth System Science Interdisciplinary Center, University of Maryland Cryospheric Science Laboratory, Goddard Space Flight Center kelly.m.brunt@nasa.gov (Based on
More informationGEOG Lecture 8. Orbits, scale and trade-offs
Environmental Remote Sensing GEOG 2021 Lecture 8 Orbits, scale and trade-offs Orbits revisit Orbits geostationary (36 000 km altitude) polar orbiting (200-1000 km altitude) Orbits revisit Orbits geostationary
More informationLecture 4b: Meteorological Satellites and Instruments. Acknowledgement: Dr. S. Kidder at Colorado State Univ.
Lecture 4b: Meteorological Satellites and Instruments Acknowledgement: Dr. S. Kidder at Colorado State Univ. US Geostationary satellites - GOES (Geostationary Operational Environmental Satellites) US
More informationATMOS 5140 Lecture 1 Chapter 1
ATMOS 5140 Lecture 1 Chapter 1 Atmospheric Radiation Relevance for Weather and Climate Solar Radiation Thermal Infrared Radiation Global Heat Engine Components of the Earth s Energy Budget Relevance for
More informationLecture 4: Radiation Transfer
Lecture 4: Radiation Transfer Spectrum of radiation Stefan-Boltzmann law Selective absorption and emission Reflection and scattering Remote sensing Importance of Radiation Transfer Virtually all the exchange
More informationPrinciples of Satellite Remote Sensing
Chapter 5 Principles of Satellite Remote Sensing Goal: Give a overview on the characteristics of satellite remote sensing. Satellites have several unique characteristics which make them particularly useful
More informationArctic Weather Every 10 Minutes: Design & Operation of ABI for PCW
Arctic Weather Every 10 Minutes: Design and Operation of ABI for PCW Dr. Paul C. Griffith and Sue Wirth 31st Space Symposium, Technical Track, Colorado Springs, Colorado This document is not subject to
More informationEarth is tilted (oblique) on its Axis!
MONDAY AM Radiation, Atmospheric Greenhouse Effect Earth's orbit around the Sun is slightly elliptical (not circular) Seasons & Days Why do we have seasons? Why aren't seasonal temperatures highest at
More informationLand Surface Temperature Measurements From the Split Window Channels of the NOAA 7 Advanced Very High Resolution Radiometer John C.
Land Surface Temperature Measurements From the Split Window Channels of the NOAA 7 Advanced Very High Resolution Radiometer John C. Price Published in the Journal of Geophysical Research, 1984 Presented
More informationImage 1: Earth from space
Image 1: Earth from space Credit: NASA Spacecraft: Apollo 17 Sensor: camera using visible light Image date: December 7, 1972 This image is a photograph of Earth taken by Harrison "Jack" Schmitt, an astronaut
More informationMODULE 2 LECTURE NOTES 1 SATELLITES AND ORBITS
MODULE 2 LECTURE NOTES 1 SATELLITES AND ORBITS 1. Introduction When a satellite is launched into the space, it moves in a well defined path around the Earth, which is called the orbit of the satellite.
More informationHistory of Aerosol Remote Sensing. Mark Smithgall Maria Zatko 597K Spring 2009
History of Aerosol Remote Sensing Mark Smithgall Maria Zatko 597K Spring 2009 Aerosol Sources Anthropogenic Biological decomposition from fertilizer and sewage treatment (ex. ammonium) Combustion of fossil
More informationMonitoring CO 2 Sources and Sinks from Space with the Orbiting Carbon Observatory (OCO)
NACP Remote Sensing Breakout Monitoring CO 2 Sources and Sinks from Space with the Orbiting Carbon Observatory (OCO) http://oco.jpl.nasa.gov David Crisp, OCO PI (JPL/Caltech) January 2007 1 of 14, Crisp,
More informationLecture 4: Meteorological Satellites and Instruments. Acknowledgement: Dr. S. Kidder at Colorado State Univ.
Lecture 4: Meteorological Satellites and Instruments Acknowledgement: Dr. S. Kidder at Colorado State Univ. Homework for the Spring Break: get some tangible, preliminary results for your final project.
More informationPreparation for FY-4A. (Submitted by Xiang Fang, CMA)
WORLD METEOROLOGICAL ORGANIZATION COMMISSION FOR BASIC SYSTEMS OPEN PROGRAMME AREA GROUP ON INTEGRATED OBSERVING SYSTEMS EXPERT TEAM ON SATELLITE UTILIZATION AND PRODUCTS ET-SUP-8/Doc. 10.3 (2.IV.2014)
More information- global radiative energy balance
(1 of 14) Further Reading: Chapter 04 of the text book Outline - global radiative energy balance - insolation and climatic regimes - composition of the atmosphere (2 of 14) Introduction Last time we discussed
More informationCGMS Baseline. Sustained contributions to the Global Observing System. Endorsed by CGMS-46 in Bengaluru, June 2018
CGMS Baseline Sustained contributions to the Global Observing System Best Practices for Achieving User Readiness for New Meteorological Satellites Endorsed by CGMS-46 in Bengaluru, June 2018 CGMS/DOC/18/1028862,
More informationWORLD S CHOICE FOR GEO IMAGING. Advanced Baseline Imager (ABI)
WORLD S CHOICE FOR GEO IMAGING Advanced Baseline Imager (ABI) MARKET-LEADING EXPERTISE DELIVERS BEST-IN-CLASS WEATHER IMAGING In cases of extreme weather such as hurricanes, typhoons, blizzards and tornadoes,
More informationGEOSC/METEO 597K Kevin Bowley Kaitlin Walsh
GEOSC/METEO 597K Kevin Bowley Kaitlin Walsh Timeline of Satellites ERS-1 (1991-2000) NSCAT (1996) Envisat (2002) RADARSAT (2007) Seasat (1978) TOPEX/Poseidon (1992-2005) QuikSCAT (1999) Jason-2 (2008)
More informationOnce a specific data set is selected, NEO will list related data sets in the panel titled Matching Datasets, which is to the right of the image.
NASA Earth Observations (NEO): A Brief Introduction NEO is a data visualization tool that allows users to explore a wealth of environmental data collected by NASA satellites. The satellites use an array
More informationIMPACT EXPERIMENTS ON GMAO DATA ASSIMILATION AND FORECAST SYSTEMS WITH MODIS WINDS DURING MOWSAP. Lars Peter Riishojgaard and Yanqiu Zhu
IMPACT EXPERIMENTS ON GMAO DATA ASSIMILATION AND FORECAST SYSTEMS WITH MODIS WINDS DURING MOWSAP Lars Peter Riishojgaard and Yanqiu Zhu Global Modeling and Assimilation Office, NASA/GSFC, Greenbelt, Maryland
More informationFundamentals of Remote Sensing
Division of Spatial Information Science Graduate School Life and Environment Sciences University of Tsukuba Fundamentals of Remote Sensing Prof. Dr. Yuji Murayama Surantha Dassanayake 10/6/2010 1 Fundamentals
More informationIce on Land! Who: Dr. Waleed Abdalati University of Colorado. Where: Greenland Ice Sheet and glaciers around the world.
Ice on Land! Who: Dr. Waleed Abdalati University of Colorado What: Studies how, why, and how fast ice sheets and glaciers are changing to understand how they will affect global ocean levels. Where: Greenland
More informationClimate Change: Global Warming Claims
Climate Change: Global Warming Claims Background information (from Intergovernmental Panel on Climate Change): The climate system is a complex, interactive system consisting of the atmosphere, land surface,
More informationRemote Sensing in Meteorology: Satellites and Radar. AT 351 Lab 10 April 2, Remote Sensing
Remote Sensing in Meteorology: Satellites and Radar AT 351 Lab 10 April 2, 2008 Remote Sensing Remote sensing is gathering information about something without being in physical contact with it typically
More informationReflectivity in Remote Sensing
Reflectivity in Remote Sensing The amount of absorbance and reflection of white light by a substance is dependent upon the molecular makeup of the substance. Humans have used dyes for years to obtain colors-
More informationP3.24 EVALUATION OF MODERATE-RESOLUTION IMAGING SPECTRORADIOMETER (MODIS) SHORTWAVE INFRARED BANDS FOR OPTIMUM NIGHTTIME FOG DETECTION
P3.24 EVALUATION OF MODERATE-RESOLUTION IMAGING SPECTRORADIOMETER (MODIS) SHORTWAVE INFRARED BANDS FOR OPTIMUM NIGHTTIME FOG DETECTION 1. INTRODUCTION Gary P. Ellrod * NOAA/NESDIS/ORA Camp Springs, MD
More informationInterpretation of Polar-orbiting Satellite Observations. Atmospheric Instrumentation
Interpretation of Polar-orbiting Satellite Observations Outline Polar-Orbiting Observations: Review of Polar-Orbiting Satellite Systems Overview of Currently Active Satellites / Sensors Overview of Sensor
More informationSoftware requirements * : Part III: 2 hrs.
Title: Product Type: Developer: Target audience: Format: Software requirements * : Data: Estimated time to complete: Mapping snow cover using MODIS Part I: The MODIS Instrument Part II: Normalized Difference
More informationSatellite observation of atmospheric dust
Satellite observation of atmospheric dust Taichu Y. Tanaka Meteorological Research Institute, Japan Meteorological Agency 11 April 2017, SDS WAS: Dust observation and modeling @WMO, Geneva Dust observations
More informationBack to basics: From Sputnik to Envisat, and beyond: The use of satellite measurements in weather forecasting and research: Part 1 A history
Back to basics: From Sputnik to Envisat, and beyond: The use of satellite measurements in weather forecasting and research: Part 1 A history Roger Brugge 1 and Matthew Stuttard 2 1 NERC Data Assimilation
More informationClimate & Earth System Science. Introduction to Meteorology & Climate. Chapter 05 SOME OBSERVING INSTRUMENTS. Instrument Enclosure.
Climate & Earth System Science Introduction to Meteorology & Climate MAPH 10050 Peter Lynch Peter Lynch Meteorology & Climate Centre School of Mathematical Sciences University College Dublin Meteorology
More informationTracking On-orbit Radiometric Accuracy and Stability of Suomi NPP VIIRS using Extended Low Latitude SNOs
Tracking On-orbit Radiometric Accuracy and Stability of Suomi NPP VIIRS using Extended Low Latitude SNOs Sirish Uprety a Changyong Cao b Slawomir Blonski c Xi Shao c Frank Padula d a CIRA, Colorado State
More information1. The frequency of an electromagnetic wave is proportional to its wavelength. a. directly *b. inversely
CHAPTER 3 SOLAR AND TERRESTRIAL RADIATION MULTIPLE CHOICE QUESTIONS 1. The frequency of an electromagnetic wave is proportional to its wavelength. a. directly *b. inversely 2. is the distance between successive
More informationLecture 3. Background materials. Planetary radiative equilibrium TOA outgoing radiation = TOA incoming radiation Figure 3.1
Lecture 3. Changes in planetary albedo. Is there a clear signal caused by aerosols and clouds? Outline: 1. Background materials. 2. Papers for class discussion: Palle et al., Changes in Earth s reflectance
More informationREVISION OF THE STATEMENT OF GUIDANCE FOR GLOBAL NUMERICAL WEATHER PREDICTION. (Submitted by Dr. J. Eyre)
WORLD METEOROLOGICAL ORGANIZATION Distr.: RESTRICTED CBS/OPAG-IOS (ODRRGOS-5)/Doc.5, Add.5 (11.VI.2002) COMMISSION FOR BASIC SYSTEMS OPEN PROGRAMME AREA GROUP ON INTEGRATED OBSERVING SYSTEMS ITEM: 4 EXPERT
More informationWhat is an Axis? An axis is an imaginary straight line that divides an object evenly. For a sphere (like a ball or a globe) the axis goes straight thr
All About Earth The only known planet with an environment to support life. What is an Axis? An axis is an imaginary straight line that divides an object evenly. For a sphere (like a ball or a globe) the
More informationSpectral Albedos. a: dry snow. b: wet new snow. c: melting old snow. a: cold MY ice. b: melting MY ice. d: frozen pond. c: melting FY white ice
Spectral Albedos a: dry snow b: wet new snow a: cold MY ice c: melting old snow b: melting MY ice d: frozen pond c: melting FY white ice d: melting FY blue ice e: early MY pond e: ageing ponds Extinction
More informationCross-calibration of Geostationary Satellite Visible-channel Imagers Using the Moon as a Common Reference
Cross-calibration of Geostationary Satellite Visible-channel Imagers Using the Moon as a Common Reference Thomas C. Stone U.S. Geological Survey, Flagstaff AZ, USA 27 30 August, 2012 Motivation The archives
More informationExtremes of Weather and the Latest Climate Change Science. Prof. Richard Allan, Department of Meteorology University of Reading
Extremes of Weather and the Latest Climate Change Science Prof. Richard Allan, Department of Meteorology University of Reading Extreme weather climate change Recent extreme weather focusses debate on climate
More informationThe ocean s overall role in climate
The ocean s overall role in climate - moderates climate in time (diurnally, annually) - redistributes heat spatially in the largescale ocean circulation - lower albedo (sea ice higher albedo) - dry atmosphere
More informationHY-2A Satellite User s Guide
National Satellite Ocean Application Service 2013-5-16 Document Change Record Revision Date Changed Pages/Paragraphs Edit Description i Contents 1 Introduction to HY-2 Satellite... 1 2 HY-2 satellite data
More informationLet s Think for a Second
Weather and Climate Let s Think for a Second Why is weather important in Ohio? Is climate important in Ohio? Spend 2 minutes sharing your thoughts with 1 partner. First, Let s Watch This. http://video.nationalgeographic.com/video/science/earthsci/climate-weather-sci/
More informationREMOTE SENSING KEY!!
REMOTE SENSING KEY!! This is a really ugly cover page I m sorry. Name Key. Score / 100 Directions: You have 50 minutes to take this test. You may use a cheatsheet (2 pages), a non-graphing calculator,
More informationName: Date: 2. The temperature of the Sun's photosphere is A) close to 1 million K. B) about 10,000 K. C) 5800 K. D) 4300 K.
Name: Date: 1. What is the Sun's photosphere? A) envelope of convective mass motion in the outer interior of the Sun B) lowest layer of the Sun's atmosphere C) middle layer of the Sun's atmosphere D) upper
More informationGraphing Sea Ice Extent in the Arctic and Antarctic
Graphing Sea Ice Extent in the Arctic and Antarctic 1. Large amounts of ice form in some seasons in the oceans near the North Pole and the South Pole (the Arctic Ocean and the Southern Ocean). This ice,
More informationLectures 7 and 8: 14, 16 Oct Sea Surface Temperature
Lectures 7 and 8: 14, 16 Oct 2008 Sea Surface Temperature References: Martin, S., 2004, An Introduction to Ocean Remote Sensing, Cambridge University Press, 454 pp. Chapter 7. Robinson, I. S., 2004, Measuring
More informationA MEDIUM EARTH ORBIT CONTELLATION FOR POLAR WIND MEASUREMENTS
A MEDIUM EARTH ORBIT CONTELLATION FOR POLAR WIND MEASUREMENTS Gerald J. Dittberner 1, Shyam N. Bajpai 1, Andrew J. Gerber, jr. 2, Richard Baron 2, Francois Rogez 2 1 U.S. National Oceanic and Atmospheric
More informationMcIDAS Activities Within The NASA Langley Research Center Clouds And Radiation Group
McIDAS Activities Within The NASA Langley Research Center Clouds And Radiation Group Kristopher Bedka Science Systems and Applications Inc @ NASA LaRC In Collaboration With (in alphabetical order) J. K.
More informationMonitoring Air Pollution from Space
Monitoring Air Pollution from Space Media Regional Training Workshop 16 th Nov 20 th Nov 2015 Shreta Ghimire International Centre for Integrated Mountain Development Kathmandu, Nepal Why do we study air
More informationPRINCIPLES OF REMOTE SENSING. Electromagnetic Energy and Spectral Signatures
PRINCIPLES OF REMOTE SENSING Electromagnetic Energy and Spectral Signatures Remote sensing is the science and art of acquiring and analyzing information about objects or phenomena from a distance. As humans,
More informationFUNDAMENTALS OF REMOTE SENSING FOR RISKS ASSESSMENT. 1. Introduction
FUNDAMENTALS OF REMOTE SENSING FOR RISKS ASSESSMENT FRANÇOIS BECKER International Space University and University Louis Pasteur, Strasbourg, France; E-mail: becker@isu.isunet.edu Abstract. Remote sensing
More information4-1 The Role of Climate
4-1 The Role of Climate 1 of 26 What Is Climate? What Is Climate? Weather is the day-to-day condition of Earth's atmosphere at a particular time and place. Climate refers to the average year-after-year
More information4-1 The Role of Climate
biology 1 of 26 2 of 26 What Is Climate? What Is Climate? Weather is the day-to-day condition of Earth's atmosphere at a particular time and place. Climate refers to the average year-after-year conditions
More informationEVALUATION OF WINDSAT SURFACE WIND DATA AND ITS IMPACT ON OCEAN SURFACE WIND ANALYSES AND NUMERICAL WEATHER PREDICTION
5.8 EVALUATION OF WINDSAT SURFACE WIND DATA AND ITS IMPACT ON OCEAN SURFACE WIND ANALYSES AND NUMERICAL WEATHER PREDICTION Robert Atlas* NOAA/Atlantic Oceanographic and Meteorological Laboratory, Miami,
More informationArctic Observing Systems Challenges, New opportunities and Integration
Arctic Observing Systems Challenges, New opportunities and Integration Japan Norway Arctic Science Week 03 June 2016 By Stein Sandven, NERSC Building an integrated Arctic Observing System Need to collect,
More informationSpace Weather Awareness in the Arctic. Torsten Neubert Head of Section for Solar System Physics
Space Weather Awareness in the Arctic Torsten Neubert Head of Section for Solar System Physics Technology in the Arctic There is significant potential Resources Tourism helped by receding ocean ice There
More informationESM 186 Environmental Remote Sensing and ESM 186 Lab Syllabus Winter 2012
ESM 186 Environmental Remote Sensing and ESM 186 Lab Syllabus Winter 2012 Instructor: Susan Ustin (slustin@ucdavis.edu) Phone: 752-0621 Office: 233 Veihmeyer Hall and 115A, the Barn Office Hours: Tuesday
More informationSimulated Radiances for OMI
Simulated Radiances for OMI document: KNMI-OMI-2000-004 version: 1.0 date: 11 February 2000 author: J.P. Veefkind approved: G.H.J. van den Oord checked: J. de Haan Index 0. Abstract 1. Introduction 2.
More informationComponents of the Climate System. Lecture 2: Earth s Climate System. Pop Quiz. Sub-components Global cycles What comes in What goes out
Lecture 2: Earth s Climate System Components of the Climate System terrestrial radiation Atmosphere Ocean solar radiation Land Energy, Water, and Biogeochemistry Cycles Sub-components Global cycles What
More informationSolar Radiation and Environmental Biophysics Geo 827, MSU Jiquan Chen Oct. 6, 2015
Solar Radiation and Environmental Biophysics Geo 827, MSU Jiquan Chen Oct. 6, 2015 1) Solar radiation basics 2) Energy balance 3) Other relevant biophysics 4) A few selected applications of RS in ecosystem
More informationTools of Astronomy Tools of Astronomy
Tools of Astronomy Tools of Astronomy The light that comes to Earth from distant objects is the best tool that astronomers can use to learn about the universe. In most cases, there is no other way to study
More informationRemote Sensing How we know what we know A Brief Tour
Remote Sensing How we know what we know A Brief Tour Dr. Erik Richard Dr. Jerald Harder LASP Richard 1 Remote Sensing The measurement of physical variables (usually light or sound) from outside of a medium
More informationFOLLOW THE ENERGY! EARTH S DYNAMIC CLIMATE SYSTEM
Investigation 1B FOLLOW THE ENERGY! EARTH S DYNAMIC CLIMATE SYSTEM Driving Question How does energy enter, flow through, and exit Earth s climate system? Educational Outcomes To consider Earth s climate
More informationLecture 2: Earth s Climate System
Lecture 2: Earth s Climate System terrestrial radiation solar radiation Atmosphere Ocean Solid Earth Land Energy, Water, and Biogeochemistry Cycles Sub-components Global cycles What comes in What goes
More informationFuture GOES (XGOHI, GOES-13/O/P, GOES-R+)
Future GOES (XGOHI, GOES-13/O/P, GOES-R+) Timothy J. Schmit NOAA/NESDIS/Satellite Applications and Research Advanced Satellite Products Branch (ASPB) Madison, WI And many others MUG Meeting October 16,
More informationRemote sensing of sea ice
Remote sensing of sea ice Ice concentration/extent Age/type Drift Melting Thickness Christian Haas Remote Sensing Methods Passive: senses shortwave (visible), thermal (infrared) or microwave radiation
More informationThe current status of FY-3D
The current status of FY-3D Xiang Fang National Satellite Meteorological Center, China Meteorological Administration (NSMC/CMA) OUTLINE Overview Key instruments onboard FY-3D Products and data service
More informationNon-meteorological Applications for Next Generation Geostationary Meteorological Satellites
Non-meteorological Applications for Next Generation Geostationary Meteorological Satellites Toshiyuki KURINO Satellite Program Division Japan Meteorological Agency Topics Advanced GEO for Earth Observation
More informationNEW CGMS BASELINE FOR THE SPACE-BASED GOS. (Submitted by the WMO Secretariat) Summary and Purpose of Document
WORLD METEOROLOGICAL ORGANIZATION COMMISSION FOR BASIC SYSTEMS OPEN PROGRAMME AREA GROUP ON INTEGRATED OBSERVING SYSTEMS EXPERT TEAM ON SATELLITE SYSTEMS ET-SAT-7/Inf. 2 (12.III.2012) ITEM: 8.1 SEVENTH
More informationSatellites, Weather and Climate Module 1: Introduction to the Electromagnetic Spectrum
Satellites, Weather and Climate Module 1: Introduction to the Electromagnetic Spectrum What is remote sensing? = science & art of obtaining information through data analysis, such that the device is not
More informationA new perspective on aerosol direct radiative effects in South Atlantic and Southern Africa
A new perspective on aerosol direct radiative effects in South Atlantic and Southern Africa Ian Chang and Sundar A. Christopher Department of Atmospheric Science University of Alabama in Huntsville, U.S.A.
More informationREMOTE SENSING TEST!!
REMOTE SENSING TEST!! This is a really ugly cover page I m sorry. Name. Score / 100 Directions: (idk if I need to put this???) You have 50 minutes to take this test. You may use a cheatsheet (2 pages),
More informationGLAS Team Member Quarterly Report
GLAS Team Member Quarterly Report Thomas A. Herring, Katherine J. Quinn, An Nguyen, Monchaya Piboon Massachusetts Institute of Technology Period: 4/1/2002 to 6/30/2002 Options for Estimating Multiple Scattering
More informationMODIS Reflective Solar Bands Calibration Algorithm and On-orbit Performance
MODIS Reflective Solar Bands Calibration Algorithm and On-orbit Performance X. (Jack) Xiong* a, J. Sun a, J. Esposito a, B. Guenther b, and W. Barnes c a Science Systems and Applications, Inc., 10210 Greenbelt
More informationEUMETSAT STATUS AND PLANS
1 EUM/TSS/VWG/15/826793 07/10/2015 EUMETSAT STATUS AND PLANS François Montagner, Marine Applications Manager, EUMETSAT WMO Polar Space Task Group 5 5-7 October 2015, DLR, Oberpfaffenhofen PSTG Strategic
More informationEyes in the Sky & Data Analysis.
Eyes in the Sky & Data Analysis How can we collect Information about Earth Climbing up Trees & Mountains Gathering Food Self Protection Understanding Surroundings By Travelling Collected Information Converted
More informationInstitute for Global Environmental Strategies: Discover Earth Program Materials
Lesson Summary Students will use either a computer interface or a thermometer and graph paper to learn about the different absorption properties of different albedos. Prior Knowledge & Skills Graphing
More informationGlobal warming and Extremes of Weather. Prof. Richard Allan, Department of Meteorology University of Reading
Global warming and Extremes of Weather Prof. Richard Allan, Department of Meteorology University of Reading Extreme weather climate change Recent extreme weather focusses debate on climate change Can we
More informationREMOTE SENSING OF THE ATMOSPHERE AND OCEANS
EAS 6145 SPRING 2007 REMOTE SENSING OF THE ATMOSPHERE AND OCEANS Instructor: Prof. Irina N. Sokolik office 2258, phone 404-894-6180 isokolik@eas.gatech.edu Meeting Time: Mondays: 3:05-4:25 PM Wednesdays:
More informationThe Dancing Lights Program
The Sun Teacher Background: The Dancing Lights Program Margaux Krahe Many people think the Sun is just a fiery yellow ball. The Sun is not actually burning because fire requires oxygen. Really, the Sun
More informationPolar Weather Prediction
Polar Weather Prediction David H. Bromwich Session V YOPP Modelling Component Tuesday 14 July 2015 A special thanks to the following contributors: Kevin W. Manning, Jordan G. Powers, Keith M. Hines, Dan
More informationSatellite Oceanography and Applications 1: Introduction, SST, Ocean color
Satellite Oceanography and Applications 1: Introduction, SST, Ocean color Ebenezer Nyadjro US Naval Research Lab RMU Summer Program (AUGUST 24-28, 2015) Objectives/Goals To know the basic methods of ocean
More informationCGMS Baseline In response to CGMS action/recommendation A45.01 HLPP reference: 1.1.8
Prepared by WGIII Agenda Item: 7.1 Discussed in WGIII CGMS Baseline In response to CGMS action/recommendation A45.01 HLPP reference: 1.1.8 In CGMS-45, Working Group III agreed to hold a review of the CGMS
More informationTowards eenvironment Prague, March GMES Space Component. Josef Aschbacher Head, ESA GMES Space Office
Towards eenvironment Prague, 25-27 March 2009 GMES Space Component Josef Aschbacher Head, ESA GMES Space Office Prague from Space Segment 2 05 Nov 2003 CNES 2003 GISAT 2007 ESA GSELAND GMES is an EU led
More informationThe VENμS mission: Earth Observation with High Spatial and Temporal Resolution Capabilities
Ben Gurion University The VENμS mission: Earth Observation with High Spatial and Temporal Resolution Capabilities G. Dedieu 1, O. Hagolle 2, A. Karnieli 3, S. Cherchali 2 P. Ferrier 2 and Y. Yaniv 4 1
More information). It is a gas produced naturally in the stratosphere where it strongly absorbs incoming
Page 1 of 6 What Determines How Much Ultraviolet Radiation Reaches the Earth s Surface? The amount of UV radiation reaching the Earth s surface varies widely around the globe and through time. Several
More informationLecture 1d: Satellite Orbits
Lecture 1d: Satellite Orbits Outline 1. Newton s Laws of Motion 2. Newton s Law of Universal Gravitation 3. Kepler s Laws 4. Putting Newton and Kepler s Laws together and applying them to the Earth-satellite
More informationLong-Term Time Series of Water Vapour Total Columns from GOME, SCIAMACHY and GOME-2
Graphics: ESA Graphics: ESA Graphics: ESA Long-Term Time Series of Water Vapour Total Columns from GOME, SCIAMACHY and GOME-2 S. Noël, S. Mieruch, H. Bovensmann, J. P. Burrows Institute of Environmental
More informationIntroduction to Atmospheric Circulation
Introduction to Atmospheric Circulation Start rotating table Cloud Fraction Dice Results from http://eos.atmos.washington.edu/erbe/ from http://eos.atmos.washington.edu/erbe/ from http://eos.atmos.washington.edu/erbe/
More informationASTR 380 Possibilities for Life in the Inner Solar System
ASTR 380 Possibilities for Life in the Inner Solar System ASTR 380 Midterm Test Results Generally people did well: 100-90 = A = 19 people 89 80 = B = 19 people 79 70 = C = 9 people 69 60 = D = 0 < 60 =
More information12a. Jupiter. Jupiter Data (Table 12-1) Jupiter Data: Numbers
12a. Jupiter Jupiter & Saturn data Jupiter & Saturn seen from the Earth Jupiter & Saturn rotation & structure Jupiter & Saturn clouds Jupiter & Saturn atmospheric motions Jupiter & Saturn rocky cores Jupiter
More informationEvapotranspiration monitoring with Meteosat Second Generation satellites: method, products and utility in drought detection.
Evapotranspiration monitoring with Meteosat Second Generation satellites: method, products and utility in drought detection. Nicolas Ghilain Royal Meteorological Institute Belgium EUMeTrain Event week
More informationChapter 1: Introduction
Chapter 1: Introduction Photogrammetry: Definition & applications What are we trying to do? Data acquisition systems 3-D viewing of 2-D imagery Automation (matching problem) Necessary tools: Image formation
More informationCourse outline, objectives, workload, projects, expectations
Course outline, objectives, workload, projects, expectations Introductions Remote Sensing Overview Elements of a remote sensing observing system 1. platform (satellite, surface, etc) 2. experimental design
More informationRadiation balance of the Earth. 6. Earth radiation balance under present day conditions. Top of Atmosphere (TOA) Radiation balance
Radiation balance of the Earth Top of Atmosphere (TOA) radiation balance 6. Earth radiation balance under present day conditions Atmospheric radiation balance: Difference between TOA and surface radiation
More informationDay 1 of Global Warming. Copyright 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Day 1 of Global Warming Copyright 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings The Atmosphere Atmosphere = the thin layer (1/100 th of Earth s diameter) of gases that surrounds
More informationClimate Modeling Dr. Jehangir Ashraf Awan Pakistan Meteorological Department
Climate Modeling Dr. Jehangir Ashraf Awan Pakistan Meteorological Department Source: Slides partially taken from A. Pier Siebesma, KNMI & TU Delft Key Questions What is a climate model? What types of climate
More informationAccuracy and Precision Requirements for Climate-Level Data Sets
Accuracy and Precision Requirements for Climate-Level Data Sets K. Thome NASA/GSFC Libya-4 Workshop Paris, France October 4-5, 2012 Accuracy requirements Commercial imagers Precision and SNR drive calibration
More information