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By Donald L. Kreider, Robert G. Kuller, Donald R. Ostberg, Fred W. Perkins, Lynn H. LOoomis
An advent to Linear research
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Extra info for An Introduction to Linear Analysis (Addison-Wesley Series in Mathematics)
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2 Water transport by the major surface currents of the oceans (Weyl, 1970). Transport rate Currents (m 3 x 10 6 s- 1 ) Antarctic circum-polar current Gulf Stream-Cape Hatteras Kuroshio current Gulf Stream-Florida Straits All the world's rivers 200-150 tOO 50 25 1 hemisphere, westward-moving South Equatorial Currents form in the same way. The South and North Equatorial Currents are separated by a current flowing in the opposite direction, the Equatorial Counter-Current. Recently an equatorial undercurrent, the Cromwell Current, has been discovered running eastwards exactly at the equator under the westward-flowing Equatorial Currents.
Based partly on satellite imagery (after Couper, 1983). 22 INTRODUCTION TO MARINE SCIENCE and must therefore keep the surface waters of the oceans well mixed. The major surface currents also affect continental climates; for example, Britain is north of Newfoundland, but has a warmer climate because the warm North Atlantic Drift flows near it. Infra-red satellite imagery and satellite tracking offree drifting buoys have shown that many of the major current flows are complex. 8). Three clockwise rings usually form north of the Gulf Stream and 8-14 anticlockwise ones to the south.
Note that the relative percentages of ions in the cyclic sea salts in river water are about the same as those in sea water (after Livingston, 1963, and Weyl, 1970). 24 are the same as those in sea water. The fall-out of salt from the whole world atmosphere is about 2 x 109 tons per year. 1, columns 3, 4). River water, therefore, contains cyclic sea salts from rain, and rock salts from rock weathering. The details of these processes are not fully understood. Residence times of water and inorganic ions The residence time of water and of salts in the ocean is important in relation to these cycles.