GEOG Lecture 8. Orbits, scale and trade-offs

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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 (35 800 km altitude) polar orbiting (200-1000 km altitude) http://www.esa.int/our_activities/launchers/types_of_orbits

Orbits: trade-offs / pros and cons Polar orbiting Polar (or near-polar) orbit inclined 85-90 to equator Typical altitude 600-700km, orbital period ~100 mins so multiple (15-20) orbits per day Majority of RS instruments e.g. MODIS, AVHRR, Landsat, SPOT, Ikonos etc.

Orbits and trade-offs: polar http://www.rap.ucar.edu/~djohnson/satellite/coverage.html

Orbits and trade-offs: polar Advantages Higher spatial resolution (<m to few km), depending on instrument and swath width Global coverage due to combination of orbit path and rotation of Earth Disadvantages Takes time to come back to point on surface e g 1 or 2 Takes time to come back to point on surface e.g. 1 or 2 days for MODIS, 16 days for Landsat

Orbits and trade-offs: polar

Orbits and trade-offs: polar Ortib Track (e.g. Terra) Live: http://www.n2yo.com/?s=25994 Static: http://www.ssec.wisc.edu/datacenter/terra/ EarthNow! Landsat Image Viewer http://earthnow.usgs.gov/

Orbits: trade-offs / pros and cons Geostationary Orbit over equator, with orbit period (by definition) of 24 hours Always in same place over surface MUCH further away then polar ~36,000km altitude

Orbits and trade-offs: Geostationary http://www.meted.ucar.edu/satmet/climate_monitoring/navmenu.php

Orbits and trade-offs: Geostationary

Orbits and trade-offs: Geostationary Advantages Always look at same part of Earth Rapid repeat time (as fast as you like) e.g. Meteosat every 15 minutes - ideal for weather monitoring/forecasting Disadvantages Much higher (36000km) altitude means lower resolution Not global coverage See same side of Earth High-latitude

Orbits and trade-offs: Geostationary METEOSAT 2 nd Gen (MSG) (geostationary orbit) 1km (equator) to 3km (worse with latitude) Views of whole Earth disk every 15 mins 30+ years METEOSAT data MSG-2 image of Northern Europe Mostly cloud free

Remember, we always have trade-offs in space, time, wavelength etc. determined by application Global coverage means broad swaths, moderate-to-low resolution Accept low spatial detail for global coverage & rapid revisit times Land cover change, deforestation, vegetation dynamics, surface reflectance, ocean and atmospheric circulation, global l carbon & hydrological cycle E.g. MODIS, MERIS

Remember, we always have trade-offs in space, time, wavelength etc. determined by application Global coverage means broad swaths, moderate-to-low resolution MODIS (Terra, Aqua) (near-polar orbit) 250m to 1km, 7 bands across visible + NIR, swath width ~2400 km, repeat 1-2 days MERIS (near-polar orbit) ~300m, 15 bands across visible + NIR, swath width ~1100 km, repeat time hours to days SeaWiFS (Sea-Viewing Wide Field-of-View Sensor) 1km resolution, 2800km swath, 16 day repeat Designed for ocean colour studies

Remember trade-offs in space, time, wavelength etc. SeaWiFS (Sea-Viewing i Wide Field-of-View Sensor) Designed for ocean colour studies 1km resolution, 2800km swath, 16 day repeat

Remember trade-offs in space, time, wavelength etc. SeaWiFS (Sea-Viewing i Wide Field-of-View Sensor) Designed for ocean colour studies 1km resolution, 2800km swath, 16 day repeat

http://oceancolor.gsfc.na htt // l f sa.gov/cgi/browse.pl SeaWiFS MODIS MERIS

Combined Chlorophyll (Ocean Colour) Combined SeaWiFS, MODIS, MERIS Dec 31, 2002

Remember trade-offs in space, time, wavelength etc. MERIS image of Californian MERIS image of Californian fires, October 2007

Remember trade-offs in space, time, wavelength etc. Local to regional Requires much higher spatial resolution (< 100m) So typically, narrower swaths (10s to 100s km) and longer repeat times (weeks to months) E.g. LandSat (polar orbit) 28m spatial, 7 bands, swath ~185km, repeat time nominally 16 days BUT optical, so clouds can be big problem E.g. IKONOS (polar orbit) 0.5m spatial, 4 bands, swath only 11 km, so requires dedicated targeting

Remember trade-offs in space, time, wavelength etc. SPOT 1-4 Relatively high resolution instrument, like Landsat 20m spatial, 60km swath, 26 day repeat IKONOS QuickBird IKONOS, QuickBird Very high resolution (<1m), narrow swath (10-15km) Limited bands, on-demand acquisition

A changing world: Earth Palm Jumeirah, UAE Images courtesy GeoEYE/SIME

RADAR revisit What does RADAR backscatter measure? Why speckles? E.g. ERS-SARSAR operates in C band, detects changes in surface heights near-polar polar, orbit100 min, repeat 35 days, swath 100km

RADAR Parameters affecting radar backscatter? Influence of frequency, polarization, roughness, incidence angle, and moistures Advantages All-weather Day and night Readings: http://www.nrcan.gc.ca/earth-sciences/geomatics/satellite-imagery-airphotos/satellite-imagery-products/educational-resources/9371 // / / /S OCS/ / C / http://earth.esa.int/applications/data_util/sardocs/spaceborne/radar_courses/ra dar_course_iii/parameters_affecting.htm

Missing Malaysian plane? http://www.n2yo.com/flight-mh370/ Also check out DigitalGlobe s Campaign: http://www.digitalglobeblog.com/2014/03/10/missingmalayairjet/

Summary Instrument characteristics determined by application How often do we need data, at what spatial and spectral resolution? Can we combine observations?? E.g. optical AND microwave? LIDAR? Polar and geostationary orbits? Constellations?