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Books on the topic 'Air surface temperature'

Author: Grafiati

Published: 4 June 2021

Last updated: 7 February 2022

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1

Jones, Philip D. Global surface air temperature variations: 1851-1984. Environmental Sciences Division at Oak Ridge National Laboratory, 1986.

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2

Hungerford, Roger D. Overstory removal and residue treatments affect soil surface, air, and soil temperature: Implications for seedling survival. U.S. Dept. of Agriculture, Forest Service, Intermountain Research Station, 1987.

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3

Labgaa, Rachid R. A model of the CO2 exchanges between biosphere and atmosphere in the tundra. Earth-Space Research Group, CRSEO -- Ellison Hall, University of California Santa Barbara, 1994.

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4

Solar technologies for buildings. Wiley, 2003.

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5

Eicker, Ursula. Solar Technologies for Buildings. John Wiley & Sons, Ltd., 2006.

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6

The N-factor in natural landscapes: Relations between air and soil-surface temperatures in the Kuparuk River Basin, Northern Alaska. C.W. Thornthwaite Associates, Laboratory of Climatology, 2000.

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7

Hypēresia, Cyprus Meteōrologikē, ed. Surface air temperatures in Cyprus. The Service, 1985.

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8

Surface air temperature anomalies for the northern hemisphere: The Russian dataset. Oak Ridge National Laboratory, 1988.

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9

Clarke, Andrew. Global temperature and life. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199551668.003.0014.

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The extreme meteorological surface air temperatures recorded to date are –89.2 oC in Antarctica, and 56.7 oC in Death Valley, California. Ground temperatures can be higher or lower than these air temperatures. The bulk of oceanic water is cold (< 4 oC) and thermally stable. Whilst data on limits to survival attract considerable attention, the thermal limits to completion of the life cycle (which define the limits to life) are much less well known. Currently identified upper thermal limits for growth are 122 oC for archaeans, 100 oC for bacteria and ~60 oC for unicellular eukaryotes. No unic

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10

Surface and upper-air meteorological data acquired during the central California ozone study (CCOS). U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Oceanic and Atmospheric Research Laboratories, Air Resources Laboratory, 2000.

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11

H, Crescenti Gennaro, and Air Resources Laboratory (U.S.), eds. Surface and upper-air meteorological data acquired during the central California ozone study (CCOS). U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Oceanic and Atmospheric Research Laboratories, Air Resources Laboratory, 2000.

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12

A, Lindemulder Elizabeth, Jovaag Kari, and United States. National Aeronautics and Space Administration., eds. Temperature-dependent daily variability of precipitable water in special sensor microwave/imager observations. National Aeronautics and Space Administration, 1995.

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13

A, Lindemulder Elizabeth, Jovaag Kari, and United States. National Aeronautics and Space Administration., eds. Temperature-dependent daily variability of precipitable water in special sensor microwave/imager observations. National Aeronautics and Space Administration, 1995.

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14

Temperature-dependent daily variability of precipitable water in special sensor microwave/imager observations. National Aeronautics and Space Administration, 1995.

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15

Temperature-dependent daily variability of precipitable water in special sensor microwave/imager observations. National Aeronautics and Space Administration, 1995.

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16

Ruzakowski, Patricia H. A. An investigation of the surface oxidation products formed in air on natural specimens of chalcopyrite as a function of temperature. 1987.

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17

Jason, Masters, and Atlantic Oceanographic and Meteorological Laboratories., eds. Continuous air and surface seawater measurements of fCO₂ on board the NOAA ship Malcolm Baldrige around-the-world cruise during 1995. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Atlantic Oceanographic and Meteorological Laboratory, 1997.

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18

Atlantic Oceanographic and Meteorological Laboratories, ed. The variability of surface-air temperature and precipitation at Miami International Airport including relationships with tropical weather system activity and El Niño: 1941-1990. Atlantic Oceanographic and Meteorological Laboratory, U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, 1994.

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19

Jet Propulsion Laboratory (U.S.), ed. 1982-1983 El Niño atlas: Nimbus-7 microwave radiometer data. National Aeronautics and Space Administration, Jet Propulsion Laboratory, California Institute of Technology, 1987.

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20

1982-1983 El Niño atlas: Nimbus-7 microwave radiometer data. National Aeronautics and Space Administration, Jet Propulsion Laboratory, California Institute of Technology, 1987.

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21

Jet Propulsion Laboratory (U.S.), ed. 1982-1983 El Niño atlas: Nimbus-7 microwave radiometer data. National Aeronautics and Space Administration, Jet Propulsion Laboratory, California Institute of Technology, 1987.

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22

Jet Propulsion Laboratory (U.S.), ed. 1982-1983 El Niño atlas: Nimbus-7 microwave radiometer data. National Aeronautics and Space Administration, Jet Propulsion Laboratory, California Institute of Technology, 1987.

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23

Dunlop, Storm. 2. The circulation of the atmosphere. Oxford University Press, 2017. http://dx.doi.org/10.1093/actrade/9780199571314.003.0002.

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‘The circulation of the atmosphere’ outlines the general model of the movement of air around the Earth. There are three circulation cells either side of the equator: the Hadley cell (nearest to the equator) and the polar cell, driven by specific temperature and pressure gradients, and the Ferrel cell between them. It describes global pressure patterns and the Coriolis effect, which results in south-westerly trade winds in the northern hemisphere and north-westerly trade winds in the southern. Also described are the Intertropical Convergence Zone, the polar easterlies, the westerlies, and how a

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24

Infrared algorithm development for ocean observations with EOS-MODIS: Technical report, semiannual, July-December 1997. National Aeronautics and Space Administration, 1997.

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25

United States. National Aeronautics and Space Administration., ed. Infrared algorithm development for ocean observations with EOS-MODIS: Technical report, semiannual, July-December 1997. National Aeronautics and Space Administration, 1997.

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26

Infrared algorithm development for ocean observations with EOS-MODIS: Technical report, semiannual, July-December 1995. National Aeronautics and Space Administration, 1995.

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27

Sheldon, Dick, and United States. National Aeronautics and Space Administration., eds. Infrared algorithm development for ocean observations with EOS-MODIS: Technical report, semiannual, July 1994-December 1994. National Aeronautics and Space Administration, 1994.

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28

United States. National Aeronautics and Space Administration., ed. Infrared algorithm development for ocean observations with EOS-MODIS: Technical report, semiannual, July-December 1995. National Aeronautics and Space Administration, 1995.

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29

Rez, Peter. Buildings. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198802297.003.0003.

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Most of the energy used by buildings goes into heating and cooling. For small buildings, such as houses, heat transfer by conduction through the sides is as much as, if not greater than, the heat transfer from air exchanges with the outside. For large buildings, such as offices and factories, the greater volume-to-surface ratio means that air exchanges are more significant. Lights, people and equipment can make significant contributions. Since the energy used depends on the difference in temperature between the inside and the outside, local climate is the most important factor that determines

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30

van der Hoeven, Frank, and Alexander Wandl. Hotterdam: How space is making Rotterdam warmer, how this affects the health of its inhabitants, and what can be done about it. TU Delft Open, 2015. http://dx.doi.org/10.47982/bookrxiv.1.

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Heat waves will occur in Rotterdam with greater frequency in the future. Those affected most will be the elderly – a group that is growing in size. In the light of the Paris heat wave of August 2003 and the one in Rotterdam in July 2006, mortality rates among the elderly in particular are likely to rise in the summer. METHOD The aim of the Hotterdam research project was to gain a better understanding of urban heat. The heat was measured and the surface energy balance modelled from that perspective. Social and physical features of the city we identified in detail with the help of satellite imag

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31

Brock, Fred V., and Scott J. Richardson. Meteorological Measurement Systems. Oxford University Press, 2001. http://dx.doi.org/10.1093/oso/9780195134513.001.0001.

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This book treats instrumentation used in meteorological surface systems, both on the synoptic scale and the mesoscale, and the instrumentation used in upper air soundings. The text includes material on first- and second-order differential equations as applied to instrument dynamic performance, and required solutions are developed. Sensor physics are emphasized in order to explain how sensors work and to explore the strengths and weaknesses of each design type. The book is organized according to sensor type and function (temperature, humidity, and wind sensors, for example), though several unif

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32

Burton, Derek, and Margaret Burton. Gas exchange. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198785552.003.0006.

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Oxygen intake for respiration, also carbon dioxide and, generally, ammonia elimination takes place across gas-exchange surfaces, usually the gills in fish. Water flows across gills, separated by the pharyngeal gill clefts, and supported by gill arches, and which possess highly folded surfaces covered by a very thin epithelium. Blood flow and water flow are separated only by the epithelium with a ‘countercurrent’ gas exchange between the two. A respiratory centre in the hind-brain is a respiratory rhythm pacemaker for the oral and pharyngeal ventilation movements creating water flow across the

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33

Xue, Yongkang, Yaoming Ma, and Qian Li. Land–Climate Interaction Over the Tibetan Plateau. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.592.

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The Tibetan Plateau (TP) is the largest and highest plateau on Earth. Due to its elevation, it receives much more downward shortwave radiation than other areas, which results in very strong diurnal and seasonal changes of the surface energy components and other meteorological variables, such as surface temperature and the convective atmospheric boundary layer. With such unique land process conditions on a distinct geomorphic unit, the TP has been identified as having the strongest land/atmosphere interactions in the mid-latitudes.Three major TP land/atmosphere interaction issues are presented

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34

Tibaldi, Stefano, and Franco Molteni. Atmospheric Blocking in Observation and Models. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.611.

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The atmospheric circulation in the mid-latitudes of both hemispheres is usually dominated by westerly winds and by planetary-scale and shorter-scale synoptic waves, moving mostly from west to east. A remarkable and frequent exception to this “usual” behavior is atmospheric blocking. Blocking occurs when the usual zonal flow is hindered by the establishment of a large-amplitude, quasi-stationary, high-pressure meridional circulation structure which “blocks” the flow of the westerlies and the progression of the atmospheric waves and disturbances embedded in them. Such blocking structures can hav

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