Appreciation of Earth Observing Systems

 

MESSR

Page history last edited by Avril Behan 2 yrs ago

MESSR (Multispectral Electronic Self-Scanning Radiometer) on MOS (Marine Observation Satellite)

Question 1

Into what general category of EOS does the instrument fall?

Multispectral


Question 2

What capture technology is used?

Pushbroom Capture Technology


Question 3

Is the sensor active or passive?

Passive


Question 4

At what wavelength(s) does the sensor function?

Band-1 0.51~0.59µm Green

Band-2 0.61~0.69µm Red

Band-3 0.72~0.80µm Near-Infrared

Band-4 0.80~1.10µm Near-Infrared


Question 5

What resolution does the sensor have – temporal and spatial?

Temporal

Revisit periods of 17 days

Spatial

The spatial resolution of the MESSR system is 50 x 502

With 100 kilometre swath to one side of the satellite track


Question 6

Is the sensor carried on an airborne or spaceborne platform? What is that platform – typically?

Spaceborne satellite – MOS - Marine Observation Satellite


Question 7

Who developed/launched/manages the sensor?

MESSR was developed, launched and now managed by the National Space Development Agency of Japan (NASDA)


Question 8

Can data be purchased from service providers?

Yes - JAXA Site


Question 9

What products are available?

Orthorectified Imagery, Stereo Views, Wind Direction, Wind Speed, GFS Marine Forecasts MOS.

Products Page

 


Question 10

At which main application areas is the sensor aimed?

Marine uses


List 2 specific projects, where they have been reported, their goals and their outcomes.

Project 1: MOS-1/1b MESSR Observations of the Antarctic Sea Ice: Ice Bands and Ice Streamers

Goal

In the Antarctic Ocean, ice bands can be often seen not only at the ice edge but also in the ice interior zone throughout the year and they extend for hundreds of kilometres in the latitudinal direction. So the goal of the project is to see if the width and spacing of ice bands tends to decrease from winter to summer.

Outcome

The MESSR data showed that the band with and spacing of the ice decreased from winter to summer. The width of an ice band is 2-6km in August and September and 0.1-0.7km in December. Then the spacing of the ice bands is 3-10km in August and September but 0.1-2km in December. But it is noted from the MESSR data that sea ice can be observed only on cloud-free conditions, which may introduce some bias in drawing general features. Furthermore, MOS-1/1b satellites have low temporal resolution, with a recurrent period of 17 days. To minimize such defects, the combined use of other satellite data such as SSM/I, NOAA AVHRR and SAR data may be helpful for future investigation.

http://www.terrapub.co.jp/journals/JO/pdf/5503/55030417.pdf

 

 

Project 2: MOS Data to Assess Water Quality in Small Lakes

Goal

The main goal of this study was to assess the technical feasibility of using MESSR data to evaluate the general water quality of small lakes, using experimental test sites like lakes in the Piedmont region of North West Italy.

Outcome

The low value observed in the green and red part of the spectrum for reflectance in the Moncenisio lake is too low for a clear mountain lake and then shows an over correction that must be changed in later approaches. Also the relative difference between the low altitude polluted lakes and the high mountain lakes is coherent with the difference in water quality that was present in previous tests proving that the MESSR data was correct.

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