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Книги з теми "Circulating water temperature"

Автор: Grafiati
Опубліковано: 30 травня 2022
Оновлено: 31 травня 2022

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1

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

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2

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

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3

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

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4

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

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5

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

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6

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

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7

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

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8

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

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9

Berberian, George A. Oceanographic conditions in the Gulf of Mexico and Straits of Florida, fall 1976. Miami, Fla: 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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10

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

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11

Berberian, George A. Oceanographic conditions in the Gulf of Mexico and Straits of Florida, Fall 1976. Miami, Fla: 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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12

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. [Knoxville, Tenn.?]: The Authority, 1993.

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13

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

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14

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

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15

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

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16

North Brazil Current rings experiment: Time series data report. Miami, Fla: 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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17

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). Miami, Fla: 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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18

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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Анотація:
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 10,000–100,000 years, insolation varies with orbital cycles, causing periodic climate variations. Opening of Southern Ocean gateways produced a circumpolar current that thermally isolated Antarctica. Declining atmospheric CO2 triggered Cenozoic glaciation. Antarctic glaciations affect global climate by lowering sea level, intensifying atmospheric circulation, and increasing planetary albedo. Ice sheets interact with ocean water, forming water masses that play a key role in global ocean circulation.
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19

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.

Повний текст джерела
Анотація:
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 10,000–100,000 years, insolation varies with orbital cycles, causing periodic climate variations. Opening of Southern Ocean gateways produced a circumpolar current that thermally isolated Antarctica. Declining atmospheric CO2 triggered Cenozoic glaciation. Antarctic glaciations affect global climate by lowering sea level, intensifying atmospheric circulation, and increasing planetary albedo. Ice sheets interact with ocean water, forming water masses that play a key role in global ocean circulation.
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20

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. Seattle, Wash: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Pacific Marine Environmental Laboratory, 1996.

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21

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. Seattle, Wash: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Pacific Marine Environmental Laboratory, 1994.

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22

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. Miami, Fla: 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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23

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

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Анотація:
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 glaciations and interglacials, such as the one in which we live. Longer still, tectonic forces operate over millions of years to produce mountain ranges like the Himalayas and continental rifts such as that in East Africa, which profoundly affect atmospheric circulation, creating deserts and monsoons. Over tens to hundreds of millions of years, plate movements gradually rearrange the continents, creating new oceans and destroying old ones, making and breaking land and sea connections, assembling and disassembling supercontinents, resulting in fundamental changes in heat transport by ocean currents. Finally, over the very long term—billions of years—climate reflects slow changes in solar luminosity as the planet heads towards a fiery Armageddon. All but two of these controls are direct or indirect consequences of plate tectonics.
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24

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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Анотація:
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 bulk of the transport of energy, momentum, and water vapor in the atmosphere, which determine the distribution of temperature, winds, and precipitation on Earth. Clouds, weather systems, and boundary layers in the oceans and atmosphere are manifestations of turbulence in the climate system. Because turbulence remains as the great unsolved problem of classical physics, we do not have a complete physical theory of climate. The aim of this summer school was to survey what is known about how turbulent flows control climate, what role they may play in climate change, and to outline where progress in this important area can be expected, given today’s computational and observational capabilities. This book reviews the state-of-the-art developments in this field and provides an essential background to future studies. All chapters are written from a pedagogical perspective, making the book accessible to masters and PhD students and all researchers wishing to enter this field. It is complemented by online video of several lectures and seminars recorded during the summer school.
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