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    Remote Sensing of Atmosphere, Land and OceanProperties from Terra

    Remote sensing of atmosphere,land and ocean properties Examples from Earth

    observations Orbit, sensors, and sampling

    characteristics

    Michael D. KingNASA Goddard Space Flight Center

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    EOS Goals & Mission Objectives

    Goals Develop an understanding of the total Earth system, and the effects of natural and

    human-induced changes on the global environment Expand scientific knowledge of the Earth system using NASAs unique capabilities

    from the vantage points of space, aircraft, and in situ platforms Disseminate information about the Earth system Support national and international environmental policy recommendationsMission Objectives Create an integrated scientific observing system that will enable multidisciplinary

    study of Earth system science Develop a comprehensive data and information system, including a data retrieval and

    processing system Acquire and assemble a global database emphasizing remote sensing measurements

    from space over a decade or more Improve predictive models of the Earth system

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    Terra Objectives

    Provide the first, consistent global snapshot of numerous importantEarth surface and atmospheric characteristics

    Improve the ability to detect the human impacts on climate by identifyingindicators, or fingerprints, of human activity that can be used todistinguish them from natural variability

    Provide measurements of the effects of clouds, aerosols, and greenhousegases on the Earths total energy balance

    Provide estimates of global terrestrial and marine productivity that willenable more accurate calculations of global carbon storage, exchangewith the atmosphere, and year-to-year variability

    Provide observations that will improve predictions of climate and ofweather at seasonal and interannual time scales Contribute to improved methods of disaster prediction, characterization,

    and risk reduction from wild fires, volcanoes, floods, and droughts

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    Terras Global Perspective

    MODIS 1-2 day global coverage in 36

    wavelengths from 250 m to 1km resolution

    MISR Stereo images at 9 look

    angles ASTER

    Hi-resolution, multi-spectralimages from 15 m to 90 mresolution, plus stereo

    MOPITT

    Global measures of CH4 & CO CERES Measures Earths shortwave,

    longwave, and net radiantenergy budget

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    ASTER

    Launched December 18, 1999

    MODIS

    CERES

    MISR

    MOPITT

    Terra

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    NASA, Terra & Aqua launches 1999, 2002 705 km polar orbits, descending (10:30

    a.m.) & ascending (1:30 p.m.) Sensor Characteristics

    36 spectral bands ranging from 0.41 to14.385 m

    cross-track scan mirror with 2330 kmswath width

    Spatial resolutions: 250 m (bands 1 - 2) 500 m (bands 3 - 7)

    1000 m (bands 8 - 36) 2% reflectance calibration accuracy onboard solar diffuser & solar diffuser

    stability monitor

    MODerate-resolution Imaging Spectroradiometer(MODIS)

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    MODIS Scan Swath

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    R = 0.65 mG = 0.56 mB = 0.47 m

    May 28, 2001

    Global Level-1B Composite Image

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    Cloud Optical Thickness(M. D. King, S. Platnick, M. Gray, E. Moody, et al. NASA GSFC,

    UMBC)

    t c

    1

    10

    70

    Level-3 MonthlyAugust 2001

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    Cloud Top Pressure(W. P. Menzel, R. Frey, K. Strabala, L. Gumley, et al. NOAA

    NESDIS, U. Wisconsin/CIMSS)Level-3 Monthly

    April 2001

    300

    400

    500

    700

    1000pc (hPa)

    900

    800

    600

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    Precipitable Water over Land & Sunglint(B. C. Gao, et al. Naval Research Laboratory)

    Level-3 MonthlyAugust 2001 q (cm)

    0.0

    2.5

    7.5

    5.0

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    Fine mode t a (0.55 m)

    0.0

    0.1

    0.2

    0.3

    0.4

    0.8

    0.7

    0.5

    0.6

    Aerosol Optical Thickness(Y. J. Kaufman, D. Tanr, D. A. Chu, L. A. Remer et al. NASA GSFC,

    University of Lille)Level-3 MonthlySeptember 2000

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    Coarse mode

    0.0

    0.1

    0.2

    0.3

    0.4t a (0.55 m)

    Aerosol Optical Thickness(Y. J. Kaufman, D. Tanr, D. A. Chu, L. A. Remer et al. NASA GSFC,

    University of Lille)Level-3 MonthlySeptember 2000

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    Global Aerosol Optical Properties

    1.0

    0.00.0 0.25 0.5

    Aerosol Optical Thickness F i n e

    A e r o s o

    l

    F r a c

    t i o n

    QuickTime an d a Sorenson Video decompressor ar e needed to see this picture.

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    MODIS Water Vapor (1 km)

    MODIS Reveals Atmospheric Moisture Details AsNever Seen Before

    GOES-8 Water Vapor (4 x 8 km)

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    MODIS Water Vapor (1 km)

    Four Panel Zoom of Cloud-Free Orographic Wavesrevealed in Water Vapor Imagery

    Shortwave Infrared Window

    Longwave Infrared WindowVisible

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    Every 100 Minutes MODIS Covers the Polar Regions

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    Every 100 Minutes MODIS Covers the Polar Regions

    QuickTime and a Video decompressor are needed to see this picture.

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    Cloud Tracked WindsWater Vapor Winds

    Winds from MODIS: An Arctic Example

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    True Color ImageSubvisible Cirrus (1.38 m)

    MODIS Detects Subvisible Cirrus

    Central AmericaApril 4, 2000

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    South America

    Surface Reflectance of South AmericaMOD09 (atmospherically corrected radiance)

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    Brazil

    Surface Reflectance of South AmericaMOD09 (atmospherically corrected radiance)

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    MODIS Land Cover Classification

    0 Water

    1 Evergreen Needleleaf Forest

    2 Evergreen Broadleaf Forest

    3 Deciduous Needleleaf Forest

    4 Deciduous Broadleaf Forest

    5 Mixed Forests

    6 Closed Shrublands

    7 Open Shrublands

    8 Woody Savannas

    9 Savannas

    10 Grasslands

    11 Permanent Wetlands

    12 Croplands

    13 Urban and Built-Up

    14 Cropland/Natural Veg. Mosaic

    15 Snow and Ice

    16 Barren or Sparsely Vegetated

    17 Tundra

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    Surface AlbedoSurface albedo = ecosystem + MOD43 (Strahler, Schaaf et al.) aggregation

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    Albedo MoviesLoops through bands 0.65, 0.86,

    1.24, 1.64, 2.1, and 3.7 mLoops through seasonal equinox

    and solstice, progressing fromJulian days 91, 173, 293, 356

    Ecosystem Color SchemePink = CropsGreen = TreesYellows = Barren/DesertsBlues = Savannas

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    MODIS Snow Cover(D. K. Hall, V. V. Salomonson, G. A. Riggs NASA GSFC)

    October 16, 2001 April 23, 2002

    Quic kTi me and a YUV420 codec decompressor are need ed to see thi s p icture.

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    Nighttime Sea Surface Temperature(O. B. Brown, P. J. Minnett, R. H. Evans University of Miami)

    -2

    5

    10

    15

    20

    3025

    C35

    Level-3 MonthlyMay 2001

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    Chlorophyll-a(K. L. Carder, R. H. Evans U. South Florida, U. Miami)

    0.01

    1.0

    10

    mg m-3 20

    0.1

    Level-3 MonthlyMay 2001

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    MODIS Sea Surface Temperature off the EastCoast of the US

    May 8, 2000

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    NASA, TRMM, Terra & Aqua launches 1997, 1999, 2002 350 km orbit (35 inclination), 705

    km polar orbits, descending (10:30a.m.) & ascending (1:30 p.m.)

    Sensor Characteristics

    3 spectral bands Shortwave (0.3-5.0 m) Window (8-12 m) Total (0.3->200 m)

    Spatial resolution: 20 km

    78 cross-track scan and 360

    azimuth biaxial scan 0.5% calibration accuracy onboard blackbodies & solar

    diffuser

    Clouds and the Earths Radiant Energy System(CERES)

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    CERES Scan Swath

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    CERES Scan Swath on Aqua

    QuickTime and a Sorenson Video decompressor are needed to see this picture.

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    CERES Measurements

    Study cloud radiative forcing andfeedbacks;

    Develop an observational baseline ofclear-sky radiative fluxes;

    Document radiant input to atmosphericand oceanic energetics models;

    Validate general circulation models; and Enhance extended-range numerical

    weather predictions

    Shortwave Flux (W m -2)

    Longwave Flux (W m-2)

    0 105 210

    100 210 320

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    Longwave (on left): Radiation emitted to space from the Earth systemShortwave (on right): Sunlight reflected back to space

    Shortwave and Longwave Radiation as Determinedfrom Data of the Terra CERES

    March 2000 May 2001

    QuickTim e and a YUV420 codec d ecompressor a re needed to s ee this pict ure.

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    NASA & MITI, Terra 705 km polar orbit, descending (10:30

    a.m.) Sensor Characteristics

    14 spectral bands ranging from 0.56 to11.3 m

    3 tiltable subsystems for acquiringstereoscopic imagery over a swathwidth of 60 km

    Spatial resolutions: 15 m (bands 1, 2, 3N, 3B) 30 m (bands 4 - 9) 90 m (bands 10 - 14)

    4% reflectance calibration accuracy(VNIR & SWIR)

    2 K brightness temperature accuracy(240-370 K)

    Advanced Spaceborne Thermal Emission & ReflectionRadiometer (ASTER)

    SWIR

    VNIR (1,2,3N)

    VNIR (3B)TIR

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    QuickTim e and a YUV420 codec decompressor are needed to see this p ic ture.

    ASTER Scan Swath

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    ASTER Spectral Bands

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    ASTER Measurements

    Spectral reflectances of theEarths surface at 15 -30 m

    Surface temperature andemissivities at 90 m

    Digital elevation maps fromstereo images

    Surface composition andvegetation mapscloud, sea ice, and polar iceproducts

    Observation of natural hazards(volcanoes, etc.)

    Color IR Shortwave IR

    Thermal IR SSTMarch 3, 2000

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    ASTER - Ji Paran, Brazil

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    ASTER - Mount St. Helens

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    NASA, EOS Terra launched in 1999 polar, descending orbits of 705 km,

    10:30 a.m. crossing Sensor Characteristics

    uses nine CCD-based push-broomcameras viewing nadir and fore & aft to70.5

    swath width of 400 km four spectral bands for each camera (36

    channels), at 443, 555, 670, & 865 nm resolutions of 275 m, 550 m, or 1.1 km

    Advantages high spectral stability 9 viewing angles helps determine aerosol

    by dependence (fixed t )

    Multi-angle Imaging SpectroRadiometer (MISR)

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    MISR Scan

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    multi-angleanimation

    Fire Animation from MISR

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    Saharan Dust Storm near Canary Islands

    February 29, 2000

    70 Forward Nadir 70 Aftward

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    MISR is being used to studyclouds and how they interactwith sunlight

    Cycling through the nine views

    of this scene of clouds overFlorida, notice the displacementof the clouds

    This is due to a geometriceffect called parallax, and nottrue motion

    Parallax Effect in MISR Images

    March 6, 2000

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    Extratropical Cyclone in the Southern OceanAugust 20, 2001

    Cloud-tracked winds cloud-top heights

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    MISR Imagery & Aerosol Optical ThicknessAngola and Namibia

    ta (0.558 m)Nadir 70 backward Multiangle

    Nadir True color RGB (672,

    558, 446 nm) 70 backward-viewing

    camera

    True color RGB Multiangle (672 nm) Red = nadir camera Green = 70 forward Blue = 70 backward

    Diner et al. (2001)

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    NASA, EOS Terra launched in 1999 polar, descending orbits of 705 km,

    10:30 a.m. crossing Sensor Characteristics

    Spectral bands:2.223-2.294 m CH4 2.323-2.345 m CO4.562-4.673 m CO

    Spatial resolution:22 km at nadir

    CO profiles:22 km x 3 km

    Swath: 640 km

    Measurement of Pollution in the Troposphere(MOPITT)

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    Quic kTim e and a YUV420 codec decompressor are needed to see this pic ture.

    MOPITT Scan Swath

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    MOPITT Measurements

    Measure and model troposphericcarbon monoxide and methaneconcentrations

    Obtain carbon monoxide profileswith 22 km x 3 km resolution

    Measure the methane column inthe troposphere Generate global maps of carbon

    monoxide and methanedistribution, and provideincreased knowledge oftropospheric chemistry

    Carbon Monoxide, March 2000

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    MOPITT CO PerspectiveThe First Year of Terra Data

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    Terras New Features Array of five Earth Science Instruments in space - hardware, software

    and maneuvers to convert the remote sensing signal into science ASTER: Thermal channels for geology and environment, stereo looks, 15-

    90 m resolutions CERES: Cloud radiative forcing, better angular sampling MISR: Multiangle views of clouds and land, BRDF, 275-1100 m resolutions

    MODIS: 250 m daily coverage for clouds and vegetation change 7 solar channels for land and aerosol 1.37 m Cirrus clouds 0.94 m water vapor fire channels and air temperature profiles at 1 km

    MOPITT : Global CO and CH4

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    earthobservatory.nasa.gov

    terra.nasa.gov

    visibleearth.nasa.gov

    Web Sites Check them out

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    MODIS Granule Flyby of the Himalayas(MOD09 Atmospherically Corrected Radiance)