Title: Marine Science IGBP Partners in the 21st Century
1Introduction to Remote Sensing
2A legacy of the Apollo Program was a commitment
to use space technology to study the Earth
3A legacy of the Apollo Program was a commitment
to use space technology to study the Earth
Today we routinely study the land, atmosphere,
and oceans from platforms in space
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6This is an infrared image of the Gulf of Maine
region that has been converted to temperature
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8The satellite remote sensing images served by
GoMOOS are from several satellites
This is a sea surface temperature (SST) image
derived from an Advanced Very High Resolution
Radiometer (AVHRR) sensor onboard a NOAA
satellite.
This is a chlorophyll (Chl) image derived from
the Sea-viewing Wide Field-of-view Sensor
(SeaWiFS) onboard the OrbView-2 satellite
operated by ORBIMAGE.
9The satellite remote sensing images served by
GoMOOS are from several satellites
This is a sea surface temperature (SST) image
derived from an Advanced Very High Resolution
Radiometer (AVHRR) sensor onboard a NOAA
satellite.
This is a chlorophyll (Chl) image derived from
the Sea-viewing Wide Field-of-view Sensor
(SeaWiFS) onboard the OrbView-2 satellite
operated by ORBIMAGE.
10This shows the coverage of the SeaWiFS in a
single day. On the next day, SeaWiFS will pass
over the blank (black) areas, thus acquiring
complete global coverage every two days but
cloudiness limits the view.
11Multispectral Capabilites
Quasi-True Color
are used to quantify the density of
biomass
- 8 bands in visible and near infrared
120
Land vegetation
Ocean chlorophyll, mg/m3
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13Global Biosphere March 2002
14Global Biosphere April 2002
15Global Biosphere May 2002
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17Half of all primary production occurs in the
ocean
where it is carried out by microalgae
(phytoplankton)
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21All satellite remote sensors detect
electromagnetic radiation (EMR)
22Multispectral Capabilites
Quasi-True Color
The ratio of the blue band (443 nm) to the green
band (555 nm) is used to derive the chlorophyll
concentration in the ocean.
23Effect of Chlorophyll on Water Reflectance Spectra
clear blue water
green water
24Coastal Zone Color Scanner (CZCS) Pigment
Algorithm
25CZCS Global Climatology (Nov. 1978Jun. 1986)
26SeaWiFS Chlorophyll Algorithm (OC4.V4, OReilly
et al., 2000)
27SeaWiFS composite image (19972000)
28For most ocean waters, phytoplankton are the
only substance affecting the color of the
water. These waters are called Case 1 waters.
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30Todays research is focusing on the coastal
ocean Unlike the Case 1 waters of the open
ocean, where phytoplankton are the only substance
affecting the color of the water, there are
numerous substances affecting the color of
coastal waters
- dissolved organic matter
- suspended sediment
- phytoplankton pigments
These are called Case 2 waters.
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32This is a true color image acquired on April
12, 1998.
33This is a true color image acquired on
September 23 1999, following passage of Hurricane
Floyd.
34The mission of the university is to educate the
next generation to use todays technologies
..for Earth and environmental sciences.
35December 1972
3630 years later
37How could we have imagined todays technology 30
years ago?
How do we prepare students for a future we cant
even imagine?
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