3 edition of An airborne study of boundary layer heat and moisture fluxes for Project FIFE found in the catalog.
An airborne study of boundary layer heat and moisture fluxes for Project FIFE
by National Aeronautics and Space Administration, National Technical Information Service, distributor in [Washington, DC, Springfield, Va.?
Written in English
|Statement||Robert D. Kelly; principal investigator.|
|Series||NASA-CR -- 190665., NASA contractor report -- NASA CR-190665.|
|Contributions||United States. National Aeronautics and Space Administration.|
|The Physical Object|
It is larger or equal to one and represents the particle elongation. We observed significant tendencies in the particles distributions in terms of IQ and β. Keywords: airborne particle, granulometry, micromorphology, Brussels environment. Keywords. airborne particle, granulometry, micromorphology, Brussels by: 6. Equally important, boundary-layer clouds are inferred from grid-averaged values (e.g. Slingo, , ; Ek and Mahrt, ; and others), but failure to predict the subgrid fraction of boundary-layer cloud cover leads to major errors in the surface energy budget and fluxes to the atmosphere, which has important implications for large-scale.
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Get this from a library. An airborne study of boundary layer heat and moisture fluxes for Project FIFE: final report. [Robert D Kelly; United States. National Aeronautics and Space Administration.]. Get this from a library. An airborne study of microwave surface sensing and boundary layer heat and moisture fluxes for Project FIFE: third semiannual (year ) status report.
[Robert D Kelly; United States. National Aeronautics and Space Administration.]. Boundary-layer heat and moisture budgets from FIFE. and the surface representativeness of turbulent heat fluxes from airborne EC measurements.
study of a non-homogeneous boundary layer. Budget Analysis of the Boundary Layer Grid Flights During FIFE Budget Analysis of the Boundary Layer Grid Flights During FIFE were designed to study the heat and moisture fluxes and.
An airborne study of boundary layer heat and moisture fluxes for Project FIFE [microform]: final report  Kelly, Robert D. [Washington, DC: National Aeronautics and Space Administration.
Finally, this paper presents a comparison between energy fluxes determined by the Bowen ratio method at one site and the average flux estimated from a boundary‐layer heat budget study for a Cited by: 4.
“the layer of air directly above the earth’s surface in which the effects of the surface (friction, heating, and cooling) are felt directly on time scales less than a day, and in which significant fluxes of momentum, heat, or matter are carried by turbulent motions on a scale of Cited by: 1.
Cambridge Core - Mathematical Modeling and Methods - Parameterization Schemes - by David J. Stensrud. An overview is given of the atmospheric boundary layer (ABL) over both continental and ocean surfaces, mainly from observational and modelling perspectives.
Much is known about ABL structure over homogeneous land surfaces, but relatively little so far as the following are concerned, (i) the cloud-topped ABL (over the sea predominantly); (ii Cited by: The budgets of water vapor and sensible heat in the convective atmospheric boundary (mixed) layer are analyzed by means of a simple slab approach adapted to steady large-scale advective conditions with radiation and cloud activity.
The entrainment flux for sensible heat is assumed to be a linear function of the surface flux. The flux of water vapor at the top of the mixed layer is Cited by: Betts AK, Desjardins RL, MacPherson JI, Kelly RD (c) Boundary-layer heat and moisture budgets from FIFE.
Bound-Lay Meteorol – Google Scholar Betts AK, Chen F, Mitchell KE, Janijic ZI () Assessment of the land-surface and boundary layer models in two operationnal versions of the NCEP Eta model using FIFE : Pavel Kabat, Martin Claussen, Paul A.
Dirmeyer, John H. Gash, Lelys Bravo de Guenni, Michel Meybe. An Introduction to Boundary Layer Meteorology Roland B.
Stull (auth.), Roland B. Stull (eds.) Part of the excitement in boundary-layer meteorology is the challenge associated with turbulent flow - one of the unsolved problems in classical physics.
The Large-Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) was an intensive scientific investigation of the tropical rainforest of Brazil and portions of adjacent countries. LBA used intensive remote-sensing techniques and ground-based experiments to investigate the atmosphere-biosphere-hydrosphere dynamics of this large tropical region.
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OAFlux: Objectively Analyzed air-sea Fluxes for the global oceans. "The OAFlux project aims to provide consistent, multi-decade, global analysis of air-sea heat, freshwater (evaporation), and momentum fluxes for use in studies of global energy budget, water cycle, atmosphere and ocean circulation, and climate.
Barbour, N.M. () Inertial navigation sensors. Lecture Series Paper 2, Low‐Cost Navigation Sensors and Integration Technology, NATO Science and Technology Organisation, Rto Educational Notes.
Page ASF CLOUD FREQUENCY DETERMINATION AT HIGH ELEVATIONS USING AN OPTICAL 35 CLOUD DETECTOR. Markus and B. Bailey, Associated Weather Services, Inc., Albany, N.Y.
A5F THE NATIONAL LIGHTNING DETECTION NEfflORK: A NEW RESOURCE FOR FOREST 38 METEOROLOGY. Lyons and D. Moon, R*SCAN Corp., Minneapolis, Minn. ASF THE. A consensus among many Air Quality (AQ) modelers is that planetary boundary layer processes are the most influential processes for surface concentrations of air pollutants.
Due to the many uncertainties intrinsically embedded in the parameterization of these processes, parameter optimization is often employed to determine an optimal set or range of values of the sensitive by: Here, footprint analysis played a key role as in the study by Kustas et al.
(), where the spatial variability of sensible and latent heat fluxes was investigated by remote sensing experiments and tower and aircraft-based observations. It was revealed that larger length scales contribute to moisture than to the sensible by:. The First ISLSCP Field Experiment (FIFE), which was a pilot study for further ISLSCP investigations, had the following specific goals (Sellers et al., ): To determine whether our understanding of biological processes on the small scale, from microns to meters, can be integrated over kilometer scales to describe interactions appropriate for.
Direct measurements of turbulent fluxes in the atmospheric surface layer (ASL) are available only at a limited number of test sites and for short time periods (Sellers and Hall ; Stull ).Efforts are well under way to evaluate these fluxes over the oceans using satellite observations (Schulz et al.
).But so far, there are no similar approaches available for land areas (Cooper et al Cited by: 9.The aim of this study was to analyse the effects of duff thickness and moisture content, and of soil mois- ture content on the transfer of heat in the soil.
The experimental design used intact soil blocks with their duff layer, subjected to connolled fires of variable very low intensities of up to kW m-I. .