Lesson 2 of 5 · Nimbus
Nimbus: develop new ways to measure Earth
8 minute lesson · 3 checks along the way
Your goal for this lessonDistinguish Nimbus research instruments, derived Earth-system products and the long-term value of historical observations.
In this lesson 3 sections · 3 checks
Using archive links & definitions
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Read & understand
Use a research series to try different measurements
NASA’s Nimbus program put seven numbered satellites into orbit between 1964 and 1978. It developed Earth-observation techniques across visible, infrared, ultraviolet and microwave wavelengths. The satellites did not all carry an identical instrument collection. A research series can test new approaches while still supplying observations that forecasters and other users find valuable.
Nimbus 1 introduced observations that helped scientists examine hurricanes during both day and night. Later members investigated additional properties of the atmosphere, oceans and land. The Nimbus 1 photograph shows a spacecraft with instruments and power equipment arranged for its observing task. It is one member of a changing research family, not a picture of every Nimbus configuration.
Check 1 of 3
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Read & understand
Connect detected radiation to a physical quantity
An infrared detects radiation in selected wavelength ranges. With calibration and an appropriate interpretation, that signal can inform estimates of cloud-top temperature. Reflected visible light and thermal infrared emission behave differently, which is why an infrared observation can remain useful after sunset. A dark or bright patch must be interpreted using the product’s actual display convention.
Nimbus 7 carried the Total Ozone Mapping Spectrometer, or TOMS, launched in 1978. Its ultraviolet observations supported estimates of total ozone above locations on Earth. An ozone map is a processed scientific product, not an ordinary color photograph of a hole. Interpreting it requires the method, quality information and understanding of what the reported quantity includes.
The Nimbus 1 spacecraft appears with extended solar panels during ground preparation. This is the first numbered Nimbus mission, not a photograph of the later Nimbus 7 ozone instrument or a map of atmospheric ozone.
Look closely
Can this photograph show how much ozone was above a location?
See what to notice
No. That quantity comes from a suitable calibrated instrument observation and retrieval, with location and acquisition information.
Check 2 of 3
10 pointsUse the reading above. You can try again without losing points.
Read & understand
Preserve an observation’s meaning as well as its pixels
Historical Nimbus imagery has been recovered from film and digitized for further study. A scan can make an old observation accessible, but accessibility alone does not make different instruments interchangeable. Researchers still need acquisition dates, location information, calibration records and knowledge of changes in sampling. Those details determine which comparisons the archive can support.
Consider a fictional study comparing a 1964 image with a modern image of the same ocean region. Before attributing an apparent difference to a physical change, match season and location, examine cloud conditions and account for the different spatial resolution. Nimbus demonstrates two lasting benefits of research missions: testing future observing techniques and leaving evidence that can answer questions beyond the original mission’s lifetime.
Check 3 of 3
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Put it together
Your lesson progress
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Explore further · Optional
Go to the source
Explore the evidence behind this lesson. These optional readings and videos open in a new tab.
- Read: NASA: the Nimbus research programCompare the explanation and its assumptions with the worked example in this lesson.
- Read: NASA: Nimbus images and the recovery of historical observationsCompare the explanation and its assumptions with the worked example in this lesson.
- Read: NASA: ozone instrument mission historyCompare the explanation and its assumptions with the worked example in this lesson.