2 edition of Day-night differences in radiosonde observations of the stratosphere and trospophere found in the catalog.
Day-night differences in radiosonde observations of the stratosphere and trospophere
National Meteorological Center (U.S.)
by Dept. of Commerce, National Oceanic and Atmospheric Administration, National Weather Service in Washington
Written in English
|Statement||Raymond M. McInturff ... [et al.], National Meteorological Center|
|Series||NOAA technical memorandum ; NWS NMC-63|
|Contributions||McInturff, R. M, United States. National Weather Service|
|The Physical Object|
|Pagination||ii, 47 p. :|
|Number of Pages||47|
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The item Day-night differences in radiosonde observations of the stratosphere and trospophere, Raymond M. McInturff [and others], National Meteorological Center represents a specific, individual, material embodiment of a distinct intellectual or artistic creation found in Indiana State Library.
differences could have come from a change in radio-sonde observations. As RW pointed out, radiosonde temperatures do not shift noticeably around this time (top of Fig.
Since night observations were not avail-able, and since day–night differences were an important aspect of the LKS analysis method, the LKS team had. Atmosphere, Upper. See also what's at your library, or elsewhere. Broader term: Atmosphere; Narrower terms: Atmospheric thermodynamics; Balloons, Pilot; Chemosphere.
A simplified method for calculating the atmospheric heating rate by absorption of solar radiation in the stratosphere and mesosphere / (Washington: National Aeronautics and Space Administration, Scientific and Technical Information Office ; Springfield, Va.: for sale by the National Technical Information Service, ), by Tatsuo Shimazaki.
Nov 01, · Diurnal variability of atmospheric stability as well as the occurrence and strength of turbulence in the troposphere and lower stratosphere at two tropical stations, Trivandrum (°N, °E) and Gadanki (°N, °E), situated in the Indian Peninsula is frecklesandhoney.com by: 5.
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night. This day-night contrast is explained by diurnal varia-tions in the photochemically driven partitioning of O and O 3 [e.g., Vaughan, ; Zommerfelds et al., ].  In contrast, few studies have considered diurnal varia-tions in the lower to middle stratosphere that contribute mainly to variations in total column ozone (see below).
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Jul 08, · The human fingerprint in global warming is evident in multiple lines of empirical evidence - in satellite measurements of outgoing infrared radiation, in surface measurements of downward infrared radiation, in the cooling stratosphere and other metrics.
Mar 06, · by Judith Curry Ted Cruz's favorite temperature data set just got a lot hotter. Sensitivity of satellite-derived tropospheric temperature trends to the diurnal cycle adjustment Carl Mears and Frank Wentz Abstract. Temperature sounding microwave radiometers flown on polar-orbiting weather satellites provide a long-term, global-scale record of upper-atmosphere temperatures, beginning in late.
in relation to atmospheric dynamics based on VIRTIS-M observations. Gorinov important indicator of the day-night circulation of the atmosphere. This work studies the distribution of the O 2 nightside airglow using both nadir (southern hemisphere) and limb (northern hemisphere) measurements made.
The organization United States, National Weather Service represents an institution, an association, or corporate body that is associated with resources found in Indiana State Library. Aug 12, · In How the “Greenhouse” Effect Works – A Guest Post and Discussion there was considerable discussion about the temperature profile in the atmosphere and how it might change with more "greenhouse" gases.
The temperature profile is also known as the lapse rate. The lapse rate has already been covered in Potential Temperature and for those new to the subject Density, Stability and.