3 edition of Barrow, Alaska automatic condensation nuclei counter and four wavelength nephelometer found in the catalog.
Air Resources Laboratories.October 1980.
|Statement||U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories|
|Publishers||U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories|
|The Physical Object|
|Pagination||xvi, 140 p. :|
|Number of Pages||43|
|2||NOAA technical memorandum ERL ARL -- 90|
nodata File Size: 5MB.
These events were strongly correlated with aerosol loading in the vertical column optical depth. To understand the conditions under which the surface data might be more representative of the column, examined the IAP data in relation to boundary layer height and mixing and found that a well-mixed boundary layer did not improve correlations between the airborne observations and those at the surface, but that the two were relatively well correlated under a range of conditions.
: Aerosol optical properties in the North China Plain during HaChi cam-paign: an in-situ optical closure study, Atmos.
This chapter outlines the history of these achievements. In addition, measurements of the widely used CCN counter are limited to supersaturations higher than 0. Due to the requirement of high ac-curacies of working conditions like temperatures, vapors and flow rates in chambers, the direct measurement ofNCCN is complex and costly Rose et al.
The ARM Aerial Facility AAF supports both routine observations such as the IAP program as well as airborne components of intensive campaigns. ARM Aerial Facility Despite the heart of the ARM Program being located on the ground, the need for airborne measurements was fully recognized from the beginning.
Aerosol optical depth at several wavelengths and backscatter and depolarization profiles from active remote sensing are measured routinely at all sites; at the SGP and Tropical Western Pacific TWP Darwin sites aerosol extinction profiles also are measured using the Raman technique.
Derivation of aerosol real refractive index, single-scattering albedo, and humidification factor using Raman lidar and aircraft size distribution. Cairns2002a : Remote sensing of atmospheric aerosols and trace gases by means of multifilter rotating shadowband radiometer. The prevailing approach was a hierarchical method of examination of processes that rested at its base on experimental verification in the form Alaska automatic condensation nuclei counter and four wavelength nephelometer radiative closure at the surface.
Ferrare, and V. Mather, and E. While reasonable agreement was found with optical properties, CCN were consistently slightly overpredicted. Ogren2005 : A three-wavelength optical extinction call for measuring aerosol light extinction and its application to determining light absorption coefficient.
In-strumentations of direct measurements of CCN number con-centration NCCN based on chamber technology are com-plex and costly; thus a simple way for measuring NCCN is needed. The coeffi-cient of determination R2 between measured and calcu-latedNCCNusing the first method is about 0.
Primary aerosol measurements made were cloud condensation nuclei CCN concentrations and aerosol size distributions above and below cloud.39L06802doi: 10. The benefits of this comprehensive suite of instruments are evident in many findings from the campaign related to the evolution of secondary organic and black carbon aerosol and their climate impacts near a major urban center e.