You can easy pick out
the radiosonde network from this type of image.
Another point: the reanalysis datasets are anchored to
the radiosonde network especially where the density of such observations is high.
Almost 50 years ago, the Quasi-Biennial Oscillation (QBO) of the winds in the equatorial stratosphere was detected due to the establishment of a global, regularly measuring
radiosonde network (Graystone, 1959; Ebdon, 1960).
The radiosonde network has been around for over 50 years, and typically most operational forecast NWP models as well as reanalysis models treat the raobs similarly.
Long - term continuity of
the radiosonde network is needed for assessing changes in water vapor, providing data with good vertical resolution, and evaluating remotely sensed water vapor fields.
Balling & Cerveny (2003) using the US
radiosonde network, find a statistically significant inverse correlation between GCR flux and low cloud cover over the continental United States.
It is of course possible that the observed humidity trends from the NCEP data are simply the result of problems with the instrumentation and operation of the global
radiosonde network from which the data are derived.
NOAA's own
radiosonde network shows no warming.
The radiosonde network has been operative since the late 1940s and substantialcontinue
This may partly be due to the coverage of sondes used in that analysis being biased to the high latitudes (since the effect of the error was principally in the tropics), or it may be because of undetected biases in
the radiosonde network itself.
The «global» reference
radiosonde network is embarrassing small.
First off, Lanzante and Free do an excellent job in really pinning down the biases (compared to satellites and models) of the standard homogenised
radiosonde networks (RATPAC2 and HadAT2).
Not exact matches
«Using more recent data and better analysis methods we have been able to re-examine the global weather balloon
network, known as
radiosondes, and have found clear indications of warming in the upper troposphere,» said lead author ARC Centre of Excellence for Climate System Science Chief Investigator Prof Steve Sherwood.
Using U.S. Weather Service data on precipitation,
radiosonde measurements of CAPE and lightning - strike counts from the National Lightning Detection
Network at the University of Albany, State University of New York (UAlbany), they concluded that 77 percent of the variations in lightning strikes could be predicted from knowing just these two parameters.
One additional piece of evidence that has been discussed frequently was the claim that the trends in UAH MSU 2LT closely matched those of the
radiosonde (balloon)
network (Christy et al, 2003).
Temperatures aloft can be measured in a number of ways, two of which are useful for climate monitoring: by
radiosondes (balloon - borne instrument packages, including thermometers, released daily or twice daily at a
network of observing stations throughout the world), and by satellite measurements of microwave radiation emitted by oxygen gas in the lower to mid-troposphere, taken with an instrument known as the Microwave Sounding Unit (MSU).5 The balloon measurements are taken at the same Greenwich mean times each day, whereas the times of day of the satellite measurements for a given location drift slowly with changes in the satellite orbits.
Location of
radiosonde stations in the World Meteorological Organization's (WMO) Global Observing System upper air
network.
For the year 2011, maps of mean (top left) CAPE from the SPARC
radiosonde data, (top right) precipitation from the NWS RFC data, (bottom left) product of the top two maps, and (bottom right) CG lightning from the National Lightning Detection
Network data.
Using U.S. Weather Service data on precipitation,
radiosonde measurements of CAPE and lightning - strike counts from the National Lightning Detection
Network at the University of Albany, State University of New York (UAlbany), they concluded that 77 percent of the variations in lightning strikes could be predicted from knowing just these two parameters.
NCEP humidity information derives ultimately from the international
network of balloon - borne
radiosondes.
Meshing the
radiosondes in a dense data
network such as the US is much easier than figuring out the North Pacific without in situ surface obs or
radiosondes.
Steve Sherwood, chief investigator for the ARC Centre of Excellence for Climate System Science and lead author for the study, explained that he and his colleague Nidhi Nishant used improved methods of analysis and more recent data to reexamine
radiosondes, or the global weather balloon
network.