MacFarlane, S.F., K.F. Evans, and A.S. Ackerman, 2002: A Bayesian algorithm for the retrieval of liquid water cloud properties
from microwave radiometer and millimeter radar data.
To reduce the variability and bias introduced into the QME AERI / LBLRTM radiance residuals, the moisture profiles from each radiosonde are scaled such that its total precipitable water vapor matches that retrieved
from the microwave radiometer (MWR), and these scaled profiles are used to drive the model.
Not exact matches
RE: Just a little piecprsteve on the credibility of the authors of the study: Study co-author Dr. Roy Spencer, a principal research scientist at the University of Alabama in Huntsville and U.S. Science Team Leader for the Advanced
Microwave Scanning
Radiometer flying on NASA's Aqua satellite, reports that real - world data
from NASA's Terra satellite contradict multiple assumptions fed into alarmist computer models.
The
microwave radiometer will measure heat radiation coming
from the Moon.
Finnish Meteorological Institute has been doing estimates of two essential sea ice parameters — namely, sea ice concentration (SIC) and sea ice thickness (SIT)-- for the Bohai Sea using a combination of a thermodynamic sea ice model and Earth observation (EO) data
from synthetic aperture radar (SAR) and
microwave radiometer.
This hindcast uses two time - varying inputs: 10 - meter wind vectors
from the atmospheric model NAVGEM (Navy Global Environmental Model, Hogan et al. 2014) run at the Fleet Numerical Meteorology and Oceanography Center (FNMOC), and analyses of ice concentrations (also produced at FNMOC)
from passive
microwave radiometer data (SSM / I).
The satellite data come
from the European Remote Sensing satellite scatterometers (ERS - 1 and ERS - 2), NASA scatterometers (NSCAT and Seawinds onboard ADEOS - 1 and QuikScat respectively), and several defense Meteorological Satellite Program (DMSP)
radiometers (Special Sensor
Microwave / Imager [SSM / I] F10 - F15).
These were based on U.S. Navy, Canadian and Danish aerial reconnaissance data and
from retrievals
from advanced very high resolution
radiometer (AVHRR), passive
microwave, and other satellite instruments
Microwave radiometers are very sensitive gauges of energy transmitted
from the Earth which scientists can use to judge the amount of water, ice or water vapour underneath the spacecraft's flight path.
The top image, made
from sea ice observations collected by the Advanced
Microwave Scanning
Radiometer (AMSR - E) Instrument on NASA's Aqua satellite, shows sea ice extent on September 19, 2010.
The Special Sensor
Microwave Imager (SSM / I)
radiometers provide brightness temperatures at three different frequencies (19.35, 37.0 and 85.5 GHz)
from which are estimated: wind speed when not raining, integrated atmospheric water vapor content, liquid water content, and a rain index.
The
Microwave Radiometer - High Frequency (MWRHF) provides time - series measurements of brightness temperatures
from two channels centered at 90 and 150 GHz.
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.
The primary sources of the post-1972 data are the hemispheric fields of sea - ice concentration
from (1) the U.S. National Ice Center (NIC), whose weekly grids (derived primarily
from satellite data) span the period 1972 - 1994, and (2) the satellite passive -
microwave grids from the Scanning Multichannel Microwave Radiometer (SMMR) / Special Sensor Microwave / Imager (SSM / I) period, 1978 - 97 (Parkinson and other
microwave grids
from the Scanning Multichannel
Microwave Radiometer (SMMR) / Special Sensor Microwave / Imager (SSM / I) period, 1978 - 97 (Parkinson and other
Microwave Radiometer (SMMR) / Special Sensor
Microwave / Imager (SSM / I) period, 1978 - 97 (Parkinson and other
Microwave / Imager (SSM / I) period, 1978 - 97 (Parkinson and others, 1999).
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 1984 image was made
from observations by the Scanning Multichannel
Microwave Radiometer (SMMR) on the Nimbus - 7 satellite.
Note: The Sea Ice Index input data comes
from the passive
microwave instrument on the DMSP satellites, but IMS uses the Advanced Microwave Scanning Radiometer - Earth Observing System (AMSR - E) instrument on the Aqua satellite from 2002
microwave instrument on the DMSP satellites, but IMS uses the Advanced
Microwave Scanning Radiometer - Earth Observing System (AMSR - E) instrument on the Aqua satellite from 2002
Microwave Scanning
Radiometer - Earth Observing System (AMSR - E) instrument on the Aqua satellite
from 2002 to 2011.
«Ocean water vapor and cloud burden trends derived
from the topex
microwave radiometer» by Brown, S.; Desai, S.; Keihm, S.; Ruf, C.
CMIS had a number of advanced capabilities that are not available
from the current operational
microwave imaging
radiometers SSM / I and SSMIS.
«Ocean water vapor and cloud burden trends derived
from the topex
microwave radiometer.»