2 edition of Development of a global model for atmospheric backscatter at C0 wavelengths found in the catalog.
Development of a global model for atmospheric backscatter at C0 wavelengths
by Institute for Atmospheric Optics and Remote Sensing, National Technical Information Service, distributor in Hampton, Va, [Springfield, Va
Written in English
|Statement||G.S. Kent ... [et al.].|
|Series||NASA contractor report -- NASA CR-175679., IFAORS technical report -- 242.|
|Contributions||Kent, Geoffrey S., United States. National Aeronautics and Space Administration.|
|The Physical Object|
Global Atmospheric Models AM4 AM4/LM4 is a new generation global atmosphere and land model that serves as a base for a new set of climate and Earth system models (CM4 and ESM4) and prediction model (SPEAR) developed at NOAA's Geophysical Fluid Dynamics Laboratory (GFDL). Proc. SPIE , Lidar and Atmospheric Sensing, pg 2 (15 September ); doi: / Read Abstract + A mobile multi-channel backscatter lidar for aerosol remote sensing is established at the Meteorological Institute of the University of Munich.
A model has been developed for simulating the effects of backscatter from scatterers advected with a mean background wind. This model has been designed to be as simple yet as realistic as possible, allowing the simulation of both spaced antenna and Doppler radars, and includes features such as aspect sensitivity, gravity wave perturbations, and turbulent by: J.E. Frederick, in Encyclopedia of Atmospheric Sciences (Second Edition), Synopsis. Atmospheric ozone absorbs incoming solar radiation, where the attenuation is greatest in the ultraviolet part of the spectrum. The absorbing properties of ozone are expressed in values of the absorption cross section, and these provide the basis for computing the transmission of the Earth's atmosphere as.
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Development of a global model for atmospheric backscatter at CO₂ wavelengths.  p. (OCoLC) Online version: Kent, G.S. Development of a global model for atmospheric backscatter at C0₂ wavelengths.
Washington, D.C.: National Aeronautics and Space Administration, Scientific and Technical Information Branch, February (OCoLC. Get this from a library. Development of a global model for atmospheric backscatter at C0₂ wavelengths.
[Geoffrey S Kent; United States. National Aeronautics and Space Administration.;]. Development of a global model for atmospheric backscatter at CO₂ wavelengths Author: Geoffrey S Kent ; Institute for Atmospheric Optics & Remote Sensing, ; United States.
Development of a global model for atmospheric backscatter at CO₂ wavelengths Author: G S Kent ; Institute for Atmospheric Optics & Remote Sensing, ; United States. The first atmospheric aerosol backscatter measurements at the rare isotope CO2 wavelength of µm were obtained in the troposphere over the Pacific Ocean in May–June Development of a global model for atmospheric backscatter at CO2 wavelengths Publication: Monthly Progress Report, 14 Mar.
- 13 Apr. Institute for Atmospheric Optics and Remote Sensing, Hampton, VA. Development of a global model for atmospheric backscatter at CO2 wavelengths. the effect of aerosol microphysical processes occurring in an aerosol plume which undergoes transport in the atmosphere. Results are presented in graphical form.
Future research directions are outlined. backscatter is evaluated by a density measurement or a model atmosphere). This allows to retrie ve the two unknowns (β a and σ a) by inverting the two independent lidar measurements.
Deﬁnition of the Global Atmosphere The principle of the Global Atmosphere conﬁguration fol-lows that set out for the atmospheric component of the HadGEM3 family in Hewitt et al. (), but extended to include short-range NWP conﬁgurations. The Global Atmosphere is a single choice of dynamical core, atmo-Cited by: The results of investigations into the problems of modeling atmospheric backscatter from aerosols, in the lowest 20 km of the atmosphere, at CO2 wavelengths are presented, along with a summary of the relevant aerosol characteristics and their variability, and a discussion of the measurement techniques and errors by: 7.
 The global distribution, sources, and propagation of atmospheric waves in the equatorial upper troposphere and lower stratosphere were investigated using an atmospheric general circulation model with TL60 resolution (‐km horizontal and ‐m vertical resolution).
The quasibiennial oscillation (QBO) with a period of ∼–2 years was simulated well without gravity wave drag Cited by: Fundamentals of Atmospheric Modeling by Mark Z. Jacobson Department of Civil & Environmental Engineering Planetary scale > 10, km Global wind systems Rossby (planetary) waves Stratospheric ozone loss Global warming.
Processes in an Atmospheric Model Figure Gas photochemistry Gas-to-particle conversion Optical depth of gases. 1 Development of the global atmospheric general circulation-chemistry model BCC-GEOS-Chem v model description and evaluation Xiao Lu1,2, Lin Zhang1,*, Tongwen Wu3,*, Michael S.
Long2, Jun Wang4, Daniel J. Jacob2, Fang Zhang3, 5 Jie Zhang3, Sebastian D. Eastham5, Lu Hu6, Lei Zhu2,7,8, Xiong Liu7, and Min Wei9 (1) Laboratory for Climate and Ocean-Atmosphere Sciences, Department File Size: 7MB.
Read "Development of a global model for atmospheric backscatter at CO2 wavelengths" by G. Kent,P. Wang,U. Farrukh,A Deepak available from Rakuten Kobo. Atmospheric backscatter vertical profiles at and µm: A comparative study Article (PDF Available) in Applied Optics 27(23) December with 28 Reads How we measure 'reads'.
The aim of research, using different types of lasers from various optical region, is to calculate differential cross scatter section and backscatter of atmosphere component in one layer from.
Space-based measurements of ozone on a global basis began with the Backscatter Ultraviolet instrument flown on Nimbus 4 in A series of similar instruments flown by National Aeronautics and Space Administration and the National Oceanic and Atmospheric Administration have documented the development of an ozone hole over the Antarctic each October, and a drop in global ozone.
Abstract. The abundance of C0 2 in the atmosphere has increased from ~ ppmv in to ~ ppmv in the s. The increase in the decade of the s is ~55% of the C0 2 release from fossil fuel combustion, estimated at Pg C yr-1, or ~40% of the total anthropogenic source, from fossil fuel combustion plus land use modification (estimated at Pg C yr-1).Cited by: 3.
The modeling of atmospheric aerosol backscattering at CO SUB 2 wavelengths. Article Atmospheric water vapor / edited by Adarash Deepak, Thomas D. Wilderson, Lothar H. Ruhnke. OPTICAL AND INFRARED PROPERTIES OF THE ATMOSPHERE too- ure a and b are now known to be too high.
The model sg~~~~~o- \ atmospheres can still be considered representative of their respective conditions up to about 50 km for temperature, \30 km for ozone densities, and the tropopause (approxi-File Size: 5MB. Development of a global model for atmospheric backscatter at C0₂ wavelengths [microform] / G.S.
Kent. Remote atmospheric profiling systems for tropospheric monitoring [microform] / J.C. Kaimal, editor; Development of data processing, interpretation and analysis system for remote sensing of .Commission on Atmospheric Chemistry and Global Pollution.
and International Aerosol Climatology Project. and International Commission on Clouds and Precipitation. The International Global Aerosol Program (IGAP) plan / edited by Adarsh Deepak and Gabor Vali A. Deepak Hampton, Va where k is the wavenumber of the radiation and K = (ε − 1)/(ε + 2) is the Clausius–Mossotti factor with ε the dielectric constant of solid ice.
The maximum extent of the particle in the s direction is D and the s coordinate is centered on the particle such that the particle lies completely within the range −D/2 ≤ s ≤ D/le A(s) is the area of particle material intersected Cited by: