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Books on the topic 'Circulating water temperature'

Author: Grafiati

Published: 30 May 2022

Last updated: 31 July 2025

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1

Gottlieb, Erik S. Currents, temperatures, and divergences observed in eastern central Lake Michigan during May-October 1984. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, 1989.

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2

F, James William, Barko John W, Tennessee Valley Authority, and United States. Army. Corps of Engineers., eds. Convective circulation during differential heating and cooling in the Minky Creek embayment of Guntersville Reservoir, data summary for 1991: Joint Agency Guntersville Project aquatic plant management. The Authority, 1993.

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3

Gottlieb, Erik S. Currents and temperatures observed in Lake Michigan from June 1982 to July 1983. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, 1989.

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4

Gottlieb, Erik S. Currents and water temperatures observed in Green Bay, Lake Michigan. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, 1990.

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5

Sullivan, Annett B. Modeling hydrodynamics, temperature, and water quality in Henry Hagg Lake, Oregon, 2000-03. U.S. Geological Survey, 2005.

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6

Sullivan, Annett B. Modeling hydrodynamics, temperature, and water quality in Henry Hagg Lake, Oregon, 2000-03. U.S. Geological Survey, 2005.

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7

Great Lakes Environmental Research Laboratory., ed. Nearshore current and temperature measurements, western Lake Michigan. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Great Lakes Environmental Research Laboratory, 1997.

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8

Great Lakes Environmental Research Laboratory., ed. Nearshore current and temperature measurements, western Lake Michigan. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Great Lakes Environmental Research Laboratory, 1997.

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9

Astrakhant͡sev, G. P. Modelirovanie techeniĭ i termicheskogo rezhima Ladozhskogo ozera. Akademii͡a nauk SSSR, In-t ozerovedenii͡a, 1988.

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10

C, Fleurant, and Atlantic Oceanographic and Meteorological Laboratories, eds. CTD/Ob2s, LADCP and XBT measurements collected aboard the R/V Seward Johnson, November-December 1998: North Brazil Current rings experiment cruise (NBC-1). U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Oceanic and Atmospheric Research Laboratories, Atlantic Oceanographic and Meteorological Laboratory, 1999.

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11

Chelton, Dudley Boyd. Central California Coastal Circulation Study: CTD observations, cruise 8401, February 1984. College of Oceanography, Oregon State University, 1987.

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12

Chelton, Dudley Boyd. Central California Coastal Circulation Study: CTD observations, cruise 8501, January 1985. College of Oceanography, Oregon State University, 1987.

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13

Chelton, Dudley Boyd. Central California Coastal Circulation Study: Drifter observations, February, July, October 1984 and January 1985. College of Oceanography, Oregon State University, 1987.

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14

Berberian, George A. Oceanographic conditions in the Gulf of Mexico and Straits of Florida, Fall 1976. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Oceanic and Atmospheric Research Laboratories, Atlantic Oceanographic and Meteorological Laboratory, 1999.

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15

Berberian, George A. Oceanographic conditions in the Gulf of Mexico and Straits of Florida, fall 1976. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Oceanic and Atmospheric Research Laboratories, Atlantic Oceanographic and Meteorological Laboratory, 2000.

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16

McTaggert, K. E. CTD/O₂ measurements collected on a climate and global change cruise (WOCE Section P13) along 165⁰E during August-October, 1992. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Pacific Marine Environmental Laboratory, 1994.

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17

C, Johnson Gregory, Taft Bruce A, and Pacific Marine Environmental Laboratory (U.S.), eds. CTD/Ob2s measurements collected on a climate and global change cruise (WOCE section P18) along 110p0sW during January-April, 1994. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Pacific Marine Environmental Laboratory, 1996.

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18

C, Johnson Gregory, Taft Bruce A, and Pacific Marine Environmental Laboratory (U.S.), eds. CTD/Ob2 smeasurements collected on a climate and global change cruise (WOCE Section P13) along 165p0sE during August-October, 1992. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Pacific Marine Environmental Laboratory, 1994.

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19

Wei, Eugene. The Tampa Bay operational forecast system (TBOFS): Model development and skill assessment. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Ocean Service, Office of Coast Survey, Coast Survey Development Laboratory, 2011.

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20

Coast Survey Development Laboratory (U.S.), ed. Three-dimensional hydrodynamic model developments for a Delaware River and Bay nowcast/forecast system. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Ocean Service, Office of Coast Survey, Coast Survey Development Laboratory, 2011.

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21

E, Peltola, and Atlantic Oceanographic and Meteorological Laboratories., eds. Chemical and hydrographic measurements on a climate and global change cruise along 24N̕ in the Atlantic Ocean WOCE section A5R(EPEAT) during January-February 1998. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Oceanic and Atmospheric Research Laboratories, Atlantic Oceanographic and Meteorological Laboratory, 2001.

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22

Dynamic Corrosion Testing of Metals in High-Temperature Water. AMPP, 1995. https://doi.org/10.5006/nace_tm0274-1995.

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Scope Materials being considered for use in, or to contain, aqueous media in high-pressure steam plants or water-cooled nuclear reactor plant systems require a measure of their rate of general corrosion under the anticipated environmental conditions. Pilot plant data are usually obtained by exposing test materials to simulated environmental conditions for various lengths of time. The general methods used for tests may be similar, but techniques and procedures usually vary widely. The lack of standardized test methods for high-temperature water corrosion testing results in data that are not alw

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23

Nearshore current and temperature measurements, western Lake Michigan. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Great Lakes Environmental Research Laboratory, 1997.

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24

North Brazil Current rings experiment: Time series data report. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Oceanic and Atmospheric Research Laboratories, Atlantic Oceanographic and Meteorological Laboratory, 2000.

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25

Lurcock, Pontus, and Fabio Florindo. Antarctic Climate History and Global Climate Changes. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190676889.013.18.

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Antarctic climate changes have been reconstructed from ice and sediment cores and numerical models (which also predict future changes). Major ice sheets first appeared 34 million years ago (Ma) and fluctuated throughout the Oligocene, with an overall cooling trend. Ice volume more than doubled at the Oligocene-Miocene boundary. Fluctuating Miocene temperatures peaked at 17–14 Ma, followed by dramatic cooling. Cooling continued through the Pliocene and Pleistocene, with another major glacial expansion at 3–2 Ma. Several interacting drivers control Antarctic climate. On timescales of 10,000–100,

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26

Lurcock, Pontus, and Fabio Florindo. Antarctic Climate History and Global Climate Changes. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190699420.013.18.

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Antarctic climate changes have been reconstructed from ice and sediment cores and numerical models (which also predict future changes). Major ice sheets first appeared 34 million years ago (Ma) and fluctuated throughout the Oligocene, with an overall cooling trend. Ice volume more than doubled at the Oligocene-Miocene boundary. Fluctuating Miocene temperatures peaked at 17–14 Ma, followed by dramatic cooling. Cooling continued through the Pliocene and Pleistocene, with another major glacial expansion at 3–2 Ma. Several interacting drivers control Antarctic climate. On timescales of 10,000–100,

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27

Livermore, Roy. Chilling Out. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198717867.003.0010.

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The Earth’s climate changes naturally on all timescales. At the short end of the spectrum—hours or days—it is affected by sudden events such as volcanic eruptions, which raise the atmospheric temperature directly, and also indirectly, by the addition of greenhouse gases such as water vapour and carbon dioxide. Over years, centuries, and millennia, climate is influenced by changes in ocean currents that, ultimately, are controlled by the geography of ocean basins. On scales of thousands to hundreds of thousands of years, the Earth’s orbit around the Sun is the crucial influence, producing glaci

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28

Bouchet, Freddy, Tapio Schneider, Antoine Venaille, and Christophe Salomon, eds. Fundamental Aspects of Turbulent Flows in Climate Dynamics. Oxford University Press, 2020. http://dx.doi.org/10.1093/oso/9780198855217.001.0001.

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This book collects the text of the lectures given at the Les Houches Summer School on “Fundamental aspects of turbulent flows in climate dynamics”, held in August 2017. Leading scientists in the fields of climate dynamics, atmosphere and ocean dynamics, geophysical fluid dynamics, physics and non-linear sciences present their views on this fast growing and interdisciplinary field of research, by venturing upon fundamental problems of atmospheric convection, clouds, large-scale circulation, and predictability. Climate is controlled by turbulent flows. Turbulent motions are responsible for the b

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