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Books on the topic 'Earch convection'

Author: Grafiati

Published: 6 September 2023

Last updated: 31 July 2025

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1

Royal Society (Great Britain). Discussion Meeting. Chemical reservoirs and convection in the earth's mantle: Papers of a discussion meeting. The Royal Society, 2002.

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2

Erickson, Gary M. A mechanism for magnetospheric substorms. National Aeronautics and Space Administration, 1994.

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3

Chassignet, Eric P. Buoyancy-driven flows. Cambridge University Press, 2012.

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4

United States. National Aeronautics and Space Administration. and Massachusetts Institute of Technology. Dept. of Earth, Atmospheric, and Planetary Sciences., eds. Lateral variation in upper mantle temperature and composition beneath mid-ocean ridges inferred from shear-wave propagation, geoid, and bathymetry. Dept. of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, 1991.

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5

A, Gnoffo Peter, and Langley Research Center, eds. Convective and radiative heating for vehicle return from the Moon and Mars. National Aeronautics and Space Administration, Langley Research Center, 1995.

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6

Wilson, Gordon R. The high latitude ionosphere-magnetosphere transition region: Simulation and data comparison. National Aeronautics and Space Administration, 1995.

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7

Gordon, Howard R. Ocean observations with EOS/MODIS: Algorithm development and post launch studies : semi-annual report (for July - December 1995). National Aeronautics and Space Administration, 1996.

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8

Gordon, Howard R. Ocean observations with EOS/MODIS: Algorithm development and post launch studies. National Aeronautics and Space Administration, 1995.

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9

United States. National Aeronautics and Space Administration., ed. Ocean observations with EOS/MODIS: Algorithm development and post launch studies : semi-annual report (for July - December 1994). National Aeronautics and Space Administration, 1995.

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10

Gordon, Howard R. Ocean observations with EOS/MODIS: Algorithm development and post launch studies : semi-annual report (for January - June 1997), contract number NAS5-31363. National Aeronautics and Space Administration, 1997.

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11

United States. National Aeronautics and Space Administration., ed. Ocean observations with EOS/MODIS: Algorithm development and post launch studies : semi-annual report (for January - June 1997), contract number NAS5-31363. National Aeronautics and Space Administration, 1997.

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12

United States. National Aeronautics and Space Administration., ed. Ocean observations with EOS/MODIS: Algorithm development and post launch studies : semi-annual report (for January-July 1995). National Aeronautics and Space Administration, 1995.

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13

United States. National Aeronautics and Space Administration., ed. Ocean observations with EOS/MODIS: Algorithm development and post launch studies : semi-annual report (for January - June 1996), contract number NAS5-31363. National Aeronautics and Space Administration, 1996.

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14

Gordon, Howard R. Ocean observations with EOS/MODIS: Algorithm development and post launch studies : semi-annual report (for January - June 1996), contract number NAS5-31363. National Aeronautics and Space Administration, 1996.

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15

Gordon, Howard R. Ocean observations with EOS/MODIS: Algorithm development and post launch studies : semi-annual report (for July - December 1994). National Aeronautics and Space Administration, 1995.

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16

United States. National Aeronautics and Space Administration., ed. Ocean observations with EOS/MODIS: Algorithm development and post launch studies : semi-annual report (for January-July 1995). National Aeronautics and Space Administration, 1995.

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17

Davies, Geoffrey F. Mantle Convection for Geologists. Cambridge University Press, 2011.

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18

Davies, Geoffrey F. Mantle Convection for Geologists. Cambridge University Press, 2011.

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19

Davies, Geoffrey F. Mantle Convection for Geologists. Cambridge University Press, 2011.

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20

Mantle Convection For Geologists. Cambridge University Press, 2011.

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21

Forte, Alessandro Marco. Mantle convection and the aspherical earth. 1985.

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22

Davies, Geoffrey F. Dynamic Earth: Plates, Plumes and Mantle Convection. Cambridge University Press, 2011.

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23

Davies, Geoffrey F. Dynamic Earth: Plates, Plumes and Mantle Convection. Cambridge University Press, 2000.

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24

Davies, Geoffrey F. Dynamic Earth: Plates, Plumes and Mantle Convection. Cambridge University Press, 2009.

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25

Davies, Geoffrey F. Dynamic Earth: Plates, Plumes and Mantle Convection. Cambridge University Press, 2000.

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26

Davies, Geoffrey F. Mantle Convection for Geologists. Cambridge University Press, 2011.

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27

Schubert, Gerald, Donald L. Turcotte, and Peter Olson. Mantle Convection in the Earth and Planets. Cambridge University Press, 2001.

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28

Schubert, Gerald, Donald L. Turcotte, and Peter Olson. Mantle Convection in the Earth and Planets. Cambridge University Press, 2009.

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29

Schubert, Gerald, Donald L. Turcotte, and Peter Olson. Mantle Convection in the Earth and Planets. Cambridge University Press, 2005.

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30

Dynamic earth: Plates, plumes, and mantle convection. Cambridge University Press, 1999.

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31

Mantle convection and the state of the Earth's interior. National Aeronautics and Space Administration, 1987.

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32

Mantle Convection in the Earth and Planets 2 Volume Set. Cambridge University Press, 2001.

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33

Mantle Convection in the Earth and Planets (Cambridge Monographs on Mechan). Cambridge University Press, 2001.

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34

Convective And Advective Heat Transfer In Geological Systems. Springer, 2008.

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35

Convection Oven Cookbook: 500 Epic Recipes for Each Convection Oven. How to Use It Easily and Which Buttons to Press at Each Step. the Foolproof Guide. Included Vegan and Gluten-Free Recipes! Independently Published, 2021.

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36

Livermore, Roy. Ups and Downs. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198717867.003.0011.

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Despite the dumbing-down of education in recent years, it would be unusual to find a ten-year-old who could not name the major continents on a map of the world. Yet how many adults have the faintest idea of the structures that exist within the Earth? Understandably, knowledge is limited by the fact that the Earth’s interior is less accessible than the surface of Pluto, mapped in 2016 by the NASA New Horizons spacecraft. Indeed, Pluto, 7.5 billion kilometres from Earth, was discovered six years earlier than the similar-sized inner core of our planet. Fortunately, modern seismic techniques enabl

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37

Furbish, David Jon. Fluid Physics in Geology. Oxford University Press, 1997. http://dx.doi.org/10.1093/oso/9780195077018.001.0001.

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Fluid Physics in Geology is aimed at geology students who are interested in understanding fluid behavior and motion in the context of a wide variety of geological problems, and who wish to pursue related work in fluid physics. The book provides an introductory treatment of the physical and dynamical behaviors of fluids by focusing first on how fluids behave in a general way, then looking more specifically at how they are involved in certain geological processes. The text is written so students may concentrate on the sections that are most relevant to their own needs. Helpful problems following

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38

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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39

Inertial currents in isotropic plasma. National Aeronautics and Space Administration, 1994.

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40

Zeitlin, Vladimir. Geophysical Fluid Dynamics. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.001.0001.

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The book explains the key notions and fundamental processes in the dynamics of the fluid envelopes of the Earth (transposable to other planets), and methods of their analysis, from the unifying viewpoint of rotating shallow-water model (RSW). The model, in its one- or two-layer versions, plays a distinguished role in geophysical fluid dynamics, having been used for around a century for conceptual understanding of various phenomena, for elaboration of approaches and methods, to be applied later in more complete models, for development and testing of numerical codes and schemes of data assimilat

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41

Ocean observations with EOS/MODIS: Algorithm development and post launch studies. National Aeronautics and Space Administration, 1995.

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42

Ocean observations with EOS/MODIS: Algorithm development and post launch studies : semi-annual report (for July - December 1995). National Aeronautics and Space Administration, 1996.

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43

Benestad, Rasmus. Climate in the Barents Region. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.655.

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The Barents Sea is a region of the Arctic Ocean named after one of its first known explorers (1594–1597), Willem Barentsz from the Netherlands, although there are accounts of earlier explorations: the Norwegian seafarer Ottar rounded the northern tip of Europe and explored the Barents and White Seas between 870 and 890 ce, a journey followed by a number of Norsemen; Pomors hunted seals and walruses in the region; and Novgorodian merchants engaged in the fur trade. These seafarers were probably the first to accumulate knowledge about the nature of sea ice in the Barents region; however, scienti

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44

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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