In storms, ice and liquid water not only are key ingredients for separating the positive and negative electrical charges that initiate a lightning strike; they also are the main features detected
by microwave sensors on satellites.
Unprecedented views of surface wind and wave fields in storms are now provided
by microwave sensors on - board polar orbiting satellites.
Not exact matches
For now, the centre is preparing for those scenarios
by incorporating data from Japan's AMSR2
microwave sensor into its sea - ice record.
In January a team led
by David Smith of Duke University demonstrated a metamaterial - based
microwave camera that requires minimal data storage and
sensors, which could replace bulkier, costlier
microwave imagers now used in some airport security booths.
In contrast, the Scripps team opted to directly correlate albedo measurements made
by NASA's CERES instrument data with observations of sea ice extent made
by the Special
Sensor Microwave Imager (SSM / I) radiometers aboard Defense Meteorological Satellite Program satellites.
Researchers from North Carolina State University have found a way to reduce the coercivity of nickel ferrite (NFO) thin films
by as much as 80 percent
by patterning the surface of the material, opening the door to more energy efficient high - frequency electronics, such as
sensors,
microwave devices and antennas.
By now, scientists have figured out how to manufacture spintronic nanogenerators,
microwave radiation detectors, and magnetic field
sensors that surpass their electronic analogs.
«Cloud water content as gauged
by the Special
Sensor Microwave / Imager (SSM / I) reaches a minimum ~ 7 days after the Forbush minimum in cosmic rays...» Svensmark et al, «Cosmic ray decreases affect atmospheric aerosols and clouds», GEOPHYSICAL RESEARCH LETTERS,
This image shows the minimum extent for 2009 as observed
by the Advanced
Microwave Scanning Radiometer for EOS (AMSR - E), a Japanese
sensor flying on NASA's Aqua satellite.
All these
sensors make measurements at critical frequencies at and above 85 gigahertz (GHz);
sensors measure
microwave emissions at 183 GHz, the signature frequency band emitted
by water vapor, making it feasible to detect frozen hydrometeors (snow, ice, and the like) in the atmosphere.
Roy and I were the first to build climate - type global temperature datasets from satellite
microwave sensors, so we learned as we went — and were aided
by others who read our papers and checked our methods.
This figure is an overlay of a lightning stroke map from WWLLN (black circles) and 91 - gigahertz brightness temperatures provided
by the Special
Sensor Microwave Imager / Sounder (SSMIS) radiometer on the low - orbit satellite DMSP F - 18.
Based on observations
by the Special
Sensor Microwave / Imagers from the Defense Meteorological Satellite Program (DMSP) satellites.
The images were made from observations
by the Special
Sensor Microwave / Imagers from the Defense Meteorological Satellite Program (DMSP) satellites.
The 2012 map was compiled from observations
by the Advanced
Microwave Scanning Radiometer 2 (AMSR - 2)
sensor on the Global Change Observation Mission 1st — Water («Shizuku») satellite, which is operated
by the Japan Aerospace Exploration Agency (JAXA).
NASA Earth Observatory image
by Jesse Allen, using data from the Advanced
Microwave Scanning Radiometer 2 AMSR - 2
sensor on the Global Change Observation Mission 1st - Water (GCOM - W1) satellite.
The
microwave sensors on the satellites do not directly measure temperature, but rather radiation given off
by oxygen in the Earth's atmosphere.
Sea ice concentration, which is independently measured and well observed
by passive
microwave satellite
sensors, gives additional important information on changes in the Antarctic environment.
Scientists from Australia, China, the US and France report in the journal Nature that they examined optical, thermal,
microwave and gravity data collected
by orbiting
sensors between 2000 and 2012.
The combined all - weather canopy surface temperature provided
by passive
microwave sensor, such as AMSR - E and hyperspectral data are also important for monitoring plants water stress for early warning.
The ice coverage has been documented since 1973
by means of passive
microwave sensors on polar orbiting satellite.
The almost linear increase in global mean temperature since 1979 has been mapped out
by Grant Foster of Tempo Analytica in the US and Stefan Rahmstorf from the Potsdam institute for Climate Impact Research, thanks to the satellite
microwave -
sensor imagery, available since that date.