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Books on the topic 'Lakes – Circulation'

Author: Grafiati
Published: 4 June 2021
Last updated: 12 February 2022

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1

Simons, T. J. The circulation of Lake Ontario during the summer of 1982 and winter of 1982/83. [Ottawa]: Environment Canada, 1989.

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2

Wold, Steven R. Water and salt balance of Great Salt Lake, Utah, and simulation of water and salt movement through the causeway. Washington: U.S. G.P.O., 1997.

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3

Loving, Brian L. Water and salt balance of Great Salt Lake, Utah, and simulation of water and salt movement through the causeway, 1987-98. Salt Lake City, Utah: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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4

Astrakhant︠s︡ev, G. P. Modelirovanie ėkosistem bolʹshikh stratifit︠s︡irovannykh ozer. Sankt-Peterburg: Nauka, 2003.

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5

L, Demin I͡U︡, ed. Gidrodinamika ozer. Sankt-Peterburg: "Nauka," S.-Peterburgskoe otd-nie, 1991.

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6

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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7

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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8

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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9

Schrader, David L. Suspended-sediment budget, flow distribution, and lake circulation for the Fox Chain of Lakes in Lake and McHenry counties, Illinois, 1997-99. De Kalb, Ill: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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10

Schrader, David L. Suspended-sediment budget, flow distribution, and lake circulation for the Fox Chain of Lakes in Lake and McHenry counties, Illinois, 1997-99. De Kalb, Ill: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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11

Schrader, David L. Suspended-sediment budget, flow distribution, and lake circulation for the Fox Chain of Lakes in Lake and McHenry counties, Illinois, 1997-99. De Kalb, Ill: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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12

Schrader, David L. Suspended-sediment budget, flow distribution, and lake circulation for the Fox Chain of Lakes in Lake and McHenry counties, Illinois, 1997-99. De Kalb, Ill: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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13

Schrader, David L. Suspended-sediment budget, flow distribution, and lake circulation for the Fox Chain of Lakes in Lake and McHenry counties, Illinois, 1997-99. De Kalb, Ill: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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14

Schrader, David L. Suspended-sediment budget, flow distribution, and lake circulation for the Fox Chain of Lakes in Lake and McHenry counties, Illinois, 1997-99. De Kalb, Ill: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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15

Schrader, David L. Suspended-sediment budget, flow distribution, and lake circulation for the Fox Chain of Lakes in Lake and McHenry Counties, Illinois, 1997-99. De Kalb, Ill: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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16

Cox, Ian Charles Spencer. The numerical modelling of vertical circulation in lakes and estuaries. Birmingham: University of Birmingham, 1985.

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17

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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18

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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19

Bührer, H. Dynamische Simulation des Bodensee-Obersees und tolerierbare Phosphor-Fracht. [Reichenau]: Internationale Gewässerschutzkommission für den Bodensee, 1993.

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20

Hall, Philip. Numerical modelling of wind-induced lake circulation. Birmingham: University of Birmingham, 1987.

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21

Smith, Gayle. Environmental assessment: Lake Hotel access and circulation improvements : Yellowstone National Park (package no. 620 FA). [Denver, Colo.?]: The Center, 1987.

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22

Smith, Gayle. Environmental assessment: Lake Hotel access and circulation improvements : Yellowstone National Park (package no. 620 FA). [Denver, Colo.?]: The Center, 1987.

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23

Branch, Canada Inland Waters. The circulation of Lake Ontario during the summer of 19882 and winter of 1982/83. Ottawa: Environment Canada, 1989.

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24

Smith, Gayle. Environmental assessment: Lake Hotel access and circulation improvements : Yellowstone National Park (package no. 620 FA). [Denver, Colo.?]: The Center, 1987.

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25

National Water Research Institute (Canada). Lakes Research Branch. The circulation of Lake Ontario during the summer of 1982 and the winter of 1982/83 / T.J. Simons and W.M. Schertzer. Burlington, Ont: Inland Waters Directorate, 1989.

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26

N, Shimaraev M., Ladeĭshchikov N. P, Verbolov V. I, and Limnologicheskiĭ institut (Akademii͡a︡ nauk SSSR), eds. Formirovanie i dinamika baĭkalʹskikh vod. Novosibirsk: Izd-vo "Nauka," Sibirskoe otd-nie, 1986.

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27

G, Bhowmik Nani, ed. Velocity distribution at two sites within the southern basin of Lake Michigan. Champaign, Ill: Illinois State Water Survey, 1991.

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28

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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29

W, Duck R., Butcher D. P, Håkanson Lars, and European Geophysical Society. General Assembly, eds. Sediment, circulation and water quality in lakes and reservoirs. Oxford [Eng.]: Pergamon, 1995.

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30

Moore, Barry C. Quantification of the role of methane in carbon cycling in a small, hypereutrophic lake. 1985.

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31

1936-, Zilitinkevich S. S., and Fedorovich E. E, eds. Modeling air-lake interaction: Physical background. Berlin: Springer-Verlag, 1991.

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32

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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33

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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34

Stephen, Lozano, and Great Lakes Environmental Research Laboratory, eds. Grain size distribution of the surface sediments collected during the Lake Michigan mass balance and environmental mapping and assessment programs. Ann Arbor, Mich: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Great Lakes Environmental Research Laboratory, 1999.

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35

C, Liu P., and Great Lakes Environmental Research Laboratory., eds. Nearshore hydrodynamics studies in western Lake Michigan, 1993-1995. 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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36

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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37

R, Stabenau Erik, Eadie Brian J, and Great Lakes Environmental Research Laboratory, eds. Particle size distribution and concentration of total suspended matter in southern Lake Michigan, January 28-February 10, 1998. Ann Arbor, Mich: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Great Lakes Environmental Research Laboratory, 1998.

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38

N, Shimaraev M., and Limnologicheskiĭ institut (Akademii͡a︡ nauk SSSR), eds. Gidrofizika i gidrologii͡a︡ vodoemov: Sbornik nauchnykh trudov. Novosibirsk: "Nauka", Sibirskoe otd-nie, 1991.

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39

Holmes, Jonathan, and Philipp Hoelzmann. The Late Pleistocene-Holocene African Humid Period as Evident in Lakes. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.531.

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From the end of the last glacial stage until the mid-Holocene, large areas of arid and semi-arid North Africa were much wetter than present, during the interval that is known as the African Humid Period (AHP). During this time, large areas were characterized by a marked increase in precipitation, an expansion of lakes, river systems, and wetlands, and the spread of grassland, shrub land, and woodland vegetation into areas that are currently much drier. Simulations with climate models indicate that the AHP was the result of orbitally forced increase in northern hemisphere summer insolation, which caused the intensification and northward expansion of the boreal summer monsoon. However, feedbacks from ocean circulation, land-surface cover, and greenhouse gases were probably also important.Lake basins and their sediment archives have provided important information about climate during the AHP, including the overall increases in precipitation and in rates, trajectories, and spatial variations in change at the beginning and the end of the interval. The general pattern is one of apparently synchronous onset of the AHP at the start of the Bølling-Allerød interstadial around 14,700 years ago, although wet conditions were interrupted by aridity during the Younger Dryas stadial. Wetter conditions returned at the start of the Holocene around 11,700 years ago covering much of North Africa and extended into parts of the southern hemisphere, including southeastern Equatorial Africa. During this time, the expansion of lakes and of grassland or shrub land vegetation over the area that is now the Sahara desert, was especially marked. Increasing aridity through the mid-Holocene, associated with a reduction in northern hemisphere summer insolation, brought about the end of the AHP by around 5000–4000 years before present. The degree to which this end was abrupt or gradual and geographically synchronous or time transgressive, remains open to debate. Taken as a whole, the lake sediment records do not support rapid and synchronous declines in precipitation and vegetation across the whole of North Africa, as some model experiments and other palaeoclimate archives have suggested. Lake sediments from basins that desiccated during the mid-Holocene may have been deflated, thus providing a misleading picture of rapid change. Moreover, different proxies of climate or environment may respond in contrasting ways to the same changes in climate. Despite this, there is evidence of rapid (within a few hundred years) termination to the AHP in some regions, with clear signs of a time-transgressive response both north to south and east to west, pointing to complex controls over the mid-Holocene drying of North Africa.
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40

J, Beven K., Chatwin Philip C, Millbank John H, and Allen Catherine M. 1954-1991, eds. Mixing and transport in the environment: A memorial volume for Catherine M. Allen (1954-1991). Chichester: J. Wiley, 1994.

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41

Beven, Keith J., and Philip C. Chatwin. Mixing and Transport in the Environment: A Memorial Volume for Catherine M. Allen (1954-1991). John Wiley & Sons Ltd (Import), 1994.

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42

Yang, Kun. Observed Regional Climate Change in Tibet over the Last Decades. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.587.

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The Tibetan Plateau (TP) is subjected to strong interactions among the atmosphere, hydrosphere, cryosphere, and biosphere. The Plateau exerts huge thermal forcing on the mid-troposphere over the mid-latitude of the Northern Hemisphere during spring and summer. This region also contains the headwaters of major rivers in Asia and provides a large portion of the water resources used for economic activities in adjacent regions. Since the beginning of the 1980s, the TP has undergone evident climate changes, with overall surface air warming and moistening, solar dimming, and decrease in wind speed. Surface warming, which depends on elevation and its horizontal pattern (warming in most of the TP but cooling in the westernmost TP), was consistent with glacial changes. Accompanying the warming was air moistening, with a sudden increase in precipitable water in 1998. Both triggered more deep clouds, which resulted in solar dimming. Surface wind speed declined from the 1970s and started to recover in 2002, as a result of atmospheric circulation adjustment caused by the differential surface warming between Asian high latitudes and low latitudes.The climate changes over the TP have changed energy and water cycles and has thus reshaped the local environment. Thermal forcing over the TP has weakened. The warming and decrease in wind speed lowered the Bowen ratio and has led to less surface sensible heating. Atmospheric radiative cooling has been enhanced, mainly through outgoing longwave emission from the warming planetary system and slightly enhanced solar radiation reflection. The trend in both energy terms has contributed to the weakening of thermal forcing over the Plateau. The water cycle has been significantly altered by the climate changes. The monsoon-impacted region (i.e., the southern and eastern regions of the TP) has received less precipitation, more evaporation, less soil moisture and less runoff, which has resulted in the general shrinkage of lakes and pools in this region, although glacier melt has increased. The region dominated by westerlies (i.e., central, northern and western regions of the TP) received more precipitation, more evaporation, more soil moisture and more runoff, which together with more glacier melt resulted in the general expansion of lakes in this region. The overall wetting in the TP is due to both the warmer and moister conditions at the surface, which increased convective available potential energy and may eventually depend on decadal variability of atmospheric circulations such as Atlantic Multi-decadal Oscillation and an intensified Siberian High. The drying process in the southern region is perhaps related to the expansion of Hadley circulation. All these processes have not been well understood.
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43

M, Cardenas Alma, and Huxley College of Environmental Studies., eds. Circulation and land use in the Guide Meridian Corridor: Wiser Lake and vicinity. Bellingham, Wash: Huxley College of Environmental Studies, Western Washington University, 1995.

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44

Meisner, Nadine. Marius Petipa. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780190659295.001.0001.

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Born two hundred years ago in Marseilles, Marius Petipa spent more than sixty years in Imperial Russia as a ballet master, serving directly under the eye of the Emperor. He became the greatest choreographer of the nineteenth century, creating a quantity of work, some of which—such as Swan Lake and The Sleeping Beauty—has survived to attract audiences all round the world. In Russia, he was revered, even if by the end of his life he had become outmoded and new ideas were circulating, culminating in the experiments of Diaghilev and the Ballets Russes. Yet even the rebels recognized his genius and their indebtedness to him. He had a lasting and profound effect, both in the Soviet Union, where ballet became an emblem of cultural prestige, and in the West, where his spiritual descendants, Diaghilev included, promulgated and extended his work. Marius Petipa: The Emperor’s Ballet Master is a survey of his life and work, before and after his arrival in St Petersburg. It is a cultural biography placing Petipa in his context. It describes the people and events around him; it traces the evolution of the aesthetics of ballet; it analyses the influences that made Petipa unique; and it examines the ways that he, in turn, influenced the course of modern ballet.
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