@prefix ns0: <http://gcmd.gsfc.nasa.gov/kms#> .
@prefix skos: <http://www.w3.org/2004/02/skos/core#> .

<https://gcmd.earthdata.nasa.gov/kms/concept/bacafa70-2fbe-4869-98bd-ba2b4a49d5f2>
  ns0:altLabel [ ] ;
  skos:definition """MAMS is a multispectral scanner which measures reflected radiation
from the Earth's surface and clouds in eight visible/near-infrared
bands, and thermal emission from the Earth's surface, clouds, and
atmospheric constituents (primarily water vapor) in four infrared
bands. The 5.0 mRa aperture of MAMS produces an instantaneous
field-of-view (IFOV) resolution of 100 m at nadir from the nominal
ER-2 altitude of 20 km. The width of the entire cross path
field-of-view scanned by the sensor is 37 km, thereby providing
detailed resolution of atmospheric and surface features across the
swath width and along the aircraft flight track. For clouds and
thunderstorm features the IFOV decreases with increasing cloud height
by a factor of (Z-20)/20, where Z is the cloud height in kilometers.

The MAMS 6.5 micrometer channel has been used to map variations in
upper tropospheric water vapor associated with a variety of
atmospheric disturbances. The upper tropospheric water vapor imagery
from VAS and the new GOES imager and sounder is very useful in the
study of upper-level dynamics of mid-latitude weather systems. This is
readily apparent in video "loops" of this from the satellite channel,
which show smooth flowing patterns associated with large-scale weather
disturbances. Changes in the brightness of the water vapor features
are related to the vertical distribution of water vapor in the middle
and upper troposphere, the integrated water vapor amount, and to a
lesser degree the temperature profile. In addition, water vapor
imagery can be used to discern small-scale variability of high clouds
(particularly cirrus) and clear air atmospheric water vapor fields. In
particular, MAMS water vapor imagery has been used to map clear air
moisture variations in a number of different applications including
lee wave situations.

The split-window channels from MAMS are similar to those from the
Advanced Very High Resolution Radiometer (AVHRR), VAS, and GOES-8/9/10
imager and sounder. The 11 micrometer channels of MAMS and VAS are
very similar, while those of AVHRR and the GOES-8/9/10 imager and
sounder are narrower and shifted toward shorter wavelengths. The 12
micrometer channel of AVHRR is positioned near 11.8 micrometer with a
bandwidth about twice that of MAMS and VAS (which are centered at
longer wavelengths). The GOES-8/9/10 imager and sounder 12 micrometer
channels are also narrow when compared to AVHRR. One of the sounder 12
micrometer channels and the imager 12 micrometer channel are centered
near 12.0 micrometer, while the other sounder channel is near 12.7
micrometers.  These 12 micrometer channels measure upwelling radiation
where water vapor and other constituent absorption (particularly, by
the Q-branch of CO2 at 12.63 micrometers) are more significant. The
spectral differences of the 12 micrometer channels produce small
differences in brightness temperatures for VAS and MAMS, but somewhat
larger differences between AVHRR and MAMS (or VAS).

More Information: "http://www.ghcc.msfc.nasa.gov/irgrp/aircraft.html"

[Adapted from NASA/MSFC/GHCC Homepage]"""@en ;
  skos:prefLabel "MAMS"@en ;
  skos:inScheme <https://gcmd.earthdata.nasa.gov/kms/concepts/concept_scheme/instruments> ;
  skos:broader <https://gcmd.earthdata.nasa.gov/kms/concept/055a79c7-61db-4250-abad-f1e09909f14c> ;
  a skos:Concept .

<https://gcmd.earthdata.nasa.gov/kms/concept/055a79c7-61db-4250-abad-f1e09909f14c>
  skos:prefLabel "Spectrometers"@en ;
  a skos:Concept ;
  skos:narrower <https://gcmd.earthdata.nasa.gov/kms/concept/bacafa70-2fbe-4869-98bd-ba2b4a49d5f2> .

