Optical properties of snow warren s. g. 1982

Author: ikfb

August undefined, 2024

WebFeb 1, 1982 · Optical Properties of Snow (Paper 1R1505) Warren, Stephen G. Publication: Reviews of Geophysics and Space Physics. Pub Date: February 1982. DOI: … Webmade of the optical properties of snow. An excel-lent review of the optical properties of snow is provided by Warren (1982). The optical proper-ties of ice biota and particulates found in the ice (Arrigo et al. 1991, Roesler and Iturriaga 1994) are also discussed briefly because of their impact on radiative transfer in sea ice. BACKGROUND By ...

Note on Certain Diurnal Variations in the Albedo of Snow and Ice

WebOptical properties of antarctic snow S.C. WARREN, T.C. CRENFELL, and P.C. MULLEN Department of Atmospheric Sciences, AK-40 University of Washington Seattle, Washington 98195 ... Warren 1982; Yamanouchi 1983). A preliminary result shows that the albedo ranges between 83 and 86 percent (calibration has not been completed yet)—low under … WebFilters: Optical-and-electrochromic-properties is [Clear All Filters] 1989. Lampert, Carl M, and R'Sue Caron-Popowich. " Electron Microscopy and Electrochemistry of Nickel Oxide Films … notes of yoga and lifestyle

Frontiers Retrieval of Dust Properties From Spectral Snow …

WebJan 1, 2009 · We will give a summary of the theory behind measuring optical snow properties and stress major points of interest. Current methods for quantifying grain size will be presented. ... Warren, S.G ... WebMar 31, 2024 · The winter of 1978-1979 will long be remembered for not only heavy snow, but bitterly cold temperatures. A winter season record of 52.9 inches of snow fell over the … WebG. Warren "Optical properties of snow" Rev. Geophys. vol. 20 no. 1 pp. 67–89 1982. 6. D. Perovich C. Polashenski A. Arntsen and C. Stwertka "Anatomy of a late spring snowfall on … how to set up a book club

The parameterization of surface albedo for sea ice and its snow …

Warren, S.Q. (1982) Optical Properties of Snow. Reviews …

WebSnow at these higher elevations and north facing slopes had not commenced surface-melting at the time of AVIR1S data acquisition. ... Warren, S. G., 1982, "Optical Properties of Snow," Reviews of Geophysics and Space Physics, vol. 20, pp. 67-89. 92. 8. FIGURES Figure 1. AVIRIS image of Mammoth Mountain with ski runs in the lower center of the ... WebMar 15, 1998 · The overall program encompassed observations of sea ice physical properties, optical properties and microwave properties, plus an extensive modeling effort. Measurements were made of an evolution sequence including young sea ice, pancake ice, snow-covered ice, first-year ice, and ponded ice. notes off intelipathWebDescribing the the snowpack is the understanding of the rate of decrease effect of crystal size and shape on snow optical properties of snow SSA, and of the factors that govern this rate. This is an enormous task (e.g. Wiscombe and Warren, 1980), has motivated studies of the SSA evolution of snow, both and approximations have been proposed. how to set up a book swap

"WebStephen G. Warren. Reviews of Geophysics, January 1982, American Geophysical Union (AGU) DOI: 10.1029/rg020i001p00067. ... Optical properties of snow, Reviews of … " - Optical properties of snow warren s. g. 1982

Optical properties of snow warren s. g. 1982

WebNov 1, 2000 · Mainly because of variability in the absorption of ice, the optical properties of snow over the solar spectrum range from nearly complete reflectance to nearly complete absorption (see Fig. 1). ... Warren 1982. S.G. Warren. Optical properties of snow. Rev. Geophys. Space Phys., 20 (1982), pp. 67-89. Google Scholar. Warren and Wiscombe 1980. WebNov 5, 2008 · Multispectral visible/near-infrared (VNIR) earth observation satellites, e.g., Ikonos, Quickbird, ALOS AVNIR-2, and DMC, usually acquire imagery in a few (3 – 5) spectral bands. Atmospheric correction is a challenging task for these images because the standard methods require at least one shortwave infrared band (around 1.6 or 2.2 µm) or …

Did you know?

WebTwo important properties of snow are surface grain-size and liquid-water fraction. The albedo of snow, which affects the energy balance, is a function of grain-size. The distribution of liquid water released from snow, which impacts the … WebSee past weather reports with the Almanac's weather history tool. Find historical weather data by zip code and access weather archives from more than 1,300 stations across the …

WebJan 20, 2024 · An approximate fit to the data reported in Colbeck ( 1982, 1986) yields a value g2 = 4.0 × 10 −2 m 2 s −1 for a liquid volume fraction θ 1 = 0.09. Snow Microstructure Recovered From Reflectance Measurements A new technique was used to recover the optical grain size from reflectance measurements ( Nolin and Dozier, 1992 ). WebZuo, Wangda, Andrew McNeil, Michael Wetter, and Eleanor S Lee. " Acceleration of Radiance for Lighting Simulation by using Parallel Computing with OpenCL." 12th International Conference of the International Building Performance Simulation Association (Building Simulation 2011). Sydney, Australia, 2011. p. 110-117. LBNL-5049E. Google Scholar ...

WebMar 1, 1996 · Warren, S.G. 1982: Optical properties of snow. Reviews of Geophysical Space Physics 20, 67-89. Google Scholar — 1984: Impurities in snow: effect on albedo and snow melt (review) . Annals of Glaciology 5, 177-79. Google … WebStephen G Warren. Professor of Atmospheric Sciences, University of Washington. No verified email. ... Optical constants of ice from the ultraviolet to the microwave: A revised compilation. SG Warren, RE Brandt ... Water resources research 18 (5), 1424-1434, 1982. 317: 1982: The changing face of Arctic snow cover: A synthesis of observed and ...

WebSnow cover detection is carried out by applying the reflectance similarities of snow and other substances in the visible red band 1 and blue band 3. Then, the threshold values are …

WebAug 1, 1998 · Atmospheric (optical thickness) and snow characteristics (grain size and type) were measured simultaneously. The ground reflectance data are compared with snow reflectance modeling results. A radiative transfer model based on the adding-doubling method is used to compute the snow reflectance. how to set up a boom arm notes office365 リンクWebIt has been measured at the snow surface and at the top of the atmosphere, but its dependence on wavelength, snow grain size, and surface roughness is still unknown. … notes ol brondbyWebWhen snow is mixed with various impurities, its optical properties are modified (Warren and Wiscombe, 1980; Warren, 1982). This process leads to an increase in the absorption of … how to set up a bookmarkWebMar 24, 1999 · Therefore, both cirrus and optically thick clouds can be directly classified and distinguished from snow at the 1.6 m wavelength (Warren, 1982). This has been clearly demonstrated using the operational Landsat Thematic Mapper satellite, which has a channel centered near 1.6 m (channel 5; 1.57-1.78 m) (Dozier, 1987; Baglio, 1989). notes off the keyboard termWebSep 1, 2005 · Just 5–10 mm of continuous snow cover raised the broadband albedo from 0.49 to 0.81, nearly as high as values measured for deep snow on the Antarctic Plateau, α = 0.83 ( Grenfell et al. 1994b ). These results are corroborated by earlier measurements of Weller (1968) on fast ice at Mawson Station. how to set up a boom micWebMeasurements of the dependence of snow albedo on wavelength, zenith angle, grain size, impurity content, and cloud cover can be interpreted in terms of single-scattering and multiscattering radiative transfer theory. Ice is very weakly absorptive in the visible minimum absorption at lambda 0.46 micrometer but has strong absorption bands in the near … notes office365 移行