2 edition of atlas of satellite-derived Northern Hemispheric snow cover frequency found in the catalog.
atlas of satellite-derived Northern Hemispheric snow cover frequency
by U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, National Weather Service in Washington, D.C
Written in English
|Statement||by Michael Matson, Chester F. Ropelewski, and Marylin S. Varnadore ; NOAA/National Environmental Satellite, Data, and Information Service ; NOAA/National Weather Service.|
|Contributions||Ropelewski, C. F., Varnadore, Marylin S., United States. National Environmental Satellite Service., United States. National Oceanic and Atmospheric Administration.|
|The Physical Object|
|Pagination||iv, 75 p. :|
|Number of Pages||75|
A low frequency record on tropospheric HCFC since the late s is available from measurements of the Southern Hemisphere Cape Grim Air Archive (CGAA) and a few Northern Hemisphere air samples (mostly from Trinidad Head) using the Advanced Global Atmospheric Gases Experiment (AGAGE) instrumentation and calibrations. Results show that declining cloud cover caused by the weakening of both the South Asian summer monsoon and local-scale atmospheric upward motion mainly led to the accelerated ground surface warming during the summers of –, whereas the decreased surface albedo caused by the snow melting was the major warming factor in winter.
Five years of continuous observations indicate that interannual variation in winter air temperature and snow cover conditions control ground thermal regimes. At sandy aeolian sites, thin snow cover and high thermal conductivity promote rapid freezing, high rates of ground cooling, and low near-surface ground temperatures ( to °C). online version of the program book. Please click the following link to download and install: When you are finished installing, please return to this window and PRESS.
Snow cover (C) Snow cover extent in the Northern Hemisphere has fallen by 7 % in March and 11 % in April during the past four decades. In winter and autumn no significant changes have occurred. Snow mass in Europe has decreased by 7 % in March from to Full text of "Satellite Altimetry for Geodesy, Geophysics and Oceanography [electronic resource]: Proceedings of the International Workshop on Satellite Altimetry, a joint workshop of IAG Section III Special Study Group SSG and IAG Section II, September .
Group-kinetic theory and modeling of atmospheric turbulence
Thames to Tahiti.
Tennessee Valley Public Power Association Project GM-1 grounding manual
The general who marched to hell
Further correspondence respecting the boundary between the British possessions in North America and the territory of Alaska, part V
Peanut snack and peanut spread
Brief submitted to the Royal Commission on Dominion-Provincial Relations.
Guide to the offshore wildlife of the northern Atlantic
Solar photochemical process engineering for production of fuels and chemicals
Ag pleez deddy!
Sizes of US marine spills (The OSIR statistical series: 30 years of oil spills)
Hospital costing and the clinician
Get this from a library. An atlas of satellite-derived Northern Hemispheric snow cover frequency. [Michael Matson; Chester F Ropelewski; Marylin S Varnadore; United States.
National Environmental Satellite Service.; United States. National Oceanic and Atmospheric Administration.]. Snow Cover: present Mean annual northern hemisphere snow cover is million average, million km2 lies over Eurasia and million km2 over North America (including Greenland).In figure 1, the variability of snow cover over the Northern Hemisphere between January and August is expressed through anomalies of individual months and twelve-month running means.
Spatial distributions of the (a) year average (–, excluding and ) of snow cover duration (SCD, in month), (b) year trend of SCD (day/year) in the Northern Hemisphere derived from the long-term satellite-derived SCE, (c) the same as (b) except that only the areas with statistically significant SCD trends (Kendall-Mankind Cited by: Seasonal Variability of Northern Hemisphere Snow cell in the digitized product has a binary value.
Cells with at least 50% of their surface covered with snow were considered snow covered. All other cells were considered snow free. In this paper we use monthly means of snow cover ex-tent calculated using a routine described fully in Robinson.
Prior to Maythe SCE CDR is based on weekly, satellite-derived Northern Hemisphere snow cover extent maps. These maps were initially produced by trained NOAA meteorologists visually interpretting photographic copies of shortwave imagery, and as time progressed, new sources of imagery as they became available.
The form Atlases represents a specific category or genre of resources found in Bates College. Associations between Continental-Scale snow cover anomalies and air mass frequencies across Eastern North America Article in International Journal of Climatology 22(12) - October The major hypothesis of this study is that continental-scale snow cover anomalies should inﬂuence air mass frequencies because of their important effects on land-surface energy budgets.
To test this hypothesis, satellite-derived Northern Hemisphere snow cover data were used in conjunction with a unique air mass classiﬁcation routine to. The study area is located in Liaoning Province, northeastern China (between 38° 43'N to 43° 2'N and ° 37'E to ° 33' E) (Figure 1), covering an area ofsquare kilomet ers.
This. Matson M, Roeplewski CF, Varnadore MS () An Atlas of Satellite-Derived Northern Hemisphere Snow Cover Frequency. National Weather Service, Wash., D.C., 75 pp Google Scholar Mauer EP, Rhoads JD, Dubayah RO, Lettenmaier DP () Evaluation of Cited by: Detection of Television Frequency Interference with Satellite Microwave Imager Observations over Oceans.
Journal of Atmospheric and Oceanic Technology, 31(12), [/jtech-d] Zou, X., Weng, F., & Yang, H. Connecting the Time Series of Microwave Sounding Observations from AMSU to ATMS for Long-Term Monitoring of. High Latitude Satellite Derived Winds From Combined Geostationary and Polar Orbiting Satellite Data Brett Hoover1, Dave Santek1, Matthew Lazzara1, Rich Dworak1, Chris Velden1, Jeff Key2, and Nick Bearson1 1Cooperative Institute for Meteorological Satellite Studies (CIMSS), Space Science and Engineering Center (SSEC), University of Wisconsin – Madison, W.
Dayton St., Madison. An Atlas of satellite-derived northern hemisphere snow cover frequency (75 pp). Washington D.C.: National Weather Service. Washington D.C.: National Weather Service. Google ScholarCited by: 1.
High Latitude Satellite Derived Winds from Combined Geostationary and Polar Orbiting Satellite Data Brett Hoover Dave Santek, Matt Lazzara, Rich Dworak, Jeff Key, Chris Velden, and Nick Bearson 11th International Winds Workshop University of Aukland, New Zealand, February THE SOLAR RADIATION ATLAS - ESRA in a nutshell 7 The European Solar Radiation Atlas (ESRA) in a nutshell 1 The ESRA-concept ESRA is a logical continuation of the European Solar Radiation Atlas of It covers a wider geo-graphical area and is backed with a data base that is considerably extended both in space and in time by: Atlas of temperature-salinity frequency distributions, North Atlantic Ocean (NOAA atlas NESDIS ; 55).
Presents a collection of plots of temperature and salinity relative frequency distributions and statistics for 5-degree squares at all standard depth levels in the Atlantic Ocean based on WORLD OCEAN DATABASE data.
Introduction. The annual cycling of water is the largest movement of a chemical substance at the surface of the earth.
Evaporation from the tropics and transport to higher latitudes not only transfers water, but also much of the absorbed heat energy (Schlesinger, ).Besides a major role in the redistribution of the earth's surface energy, water vapor plays a key role in regulating the Cited by: Visit to get more information about this book, to buy it in print, or to download it as a free PDF.
image All images latest This Just In Flickr Commons Occupy Wall Street Flickr Cover Art USGS Maps. Metropolitan Museum. Top Full text of "EOS Data Products Handbook" See other formats.
A discussion of the accuracy of NOAA satellite-derived global seasonal snow cover measurements. Large Scale Effects of Seasonal Snow Cover, International Association of Hydrological Sciences PublicationThe important part, it also has this listed: Pielke, R.A., Sr., G.E. Liston, W.L. Chapman & D.A.
Robinson (). 9 Climate Variability and Change: Seasonal to Centennial INPUT SUMMARY. Earth system science—theory, observations, and modeling—of the coupled atmosphere-ocean-biosphere-cryosphere system ()—has advanced significantly in recent is now a better recognition of the principal gaps in knowledge that need to be filled in order to understand and predict both the natural.
by Judith Curry Liu, Curry et al. have a new paper published in PNAS entitled "Impact of Declining Arctic Sea Ice on Winter Snowfall." Impact of Declining Arctic Sea Ice on Winter Snowfall Jiping Liu Judith A. Curry Huijun Wang Mirong Song Radley M.
Horton Abstract. While the Arctic region has.Alexeev et al. (), for example, showed that polar amplification arises in climate models of “aquaplanets” (i.e., systems with no sea ice or snow cover). The complexity of the processes and feedbacks challenges observational assessments (and indeed has motivated special field programs such as SHEBA, described in the appendix, and MOSAiC).Author: John E.
Walsh, David H. Bromwich, James. E. Overland, Mark C. Serreze, Kevin R. Wood.