作者：
QUARLES, GILFORD G.THE AUTHOR born December 24
1909 in Charlottesville Virginia. Graduated from the University of Virginia with a B.S. in electrical engineering in 1930 and Ph.D. in physics 1934. Taught physics at the University of Alabama and Furman University until 1944 when he joined the staff of the Harvard Underwater Sound Laboratory. At the end of the War moved to Penn State as project engineer in the newly established Ordnance Research Laboratory and became Assistant Director in 1947 and Director in 1952. In these capacities he has conducted and guided research and development in various fields related to the Navy's torpedo program including acoustics electronics hydrodynamics homing systems control and propulsion. He is a member of AIEE ASEE American Physical Society American Ordnance Association Tau Beta Pi and Sigma Xi.
Time and energy characteristics of x rays from fission fragments of thermally fissioned U235 and Pu239 were investigated. The timing data were obtained electronically using amplitude-conversion techniques while the en...
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作者：
HARRISON, CHARLES W.COMMANDER CHARLES W. HARRISON
JR. USN attended the U. S. Naval Academy Preparatory School the U. S. Coast Guard Academy and the University of Virginia where in 1939 he received the S.B. degree in Engineering and in 1940 the degree of Electrical Engineer. In 1942 he was graduated with the S.M. degree in Communication Engineering from Cruft Laboratory Harvard University and that summer completed the Navy Course in Radar Engineering at Massachusetts Institute of Technology. Subsequently for several years he was engaged in lecturing to officers of the Armed Forces assigned to the radar schools at Harvard and Princeton Universities. He has had four tours of duty in the Electronics Design and Development Division Bureau of Ships two at the U.S. Naval Research Laboratoryone at the Signal Corps Engineering Laboratories (Evans Signal Laboratory)and one at the Philadelphia Naval Shipyard. His experience includes amateur
naval and broadcasting operation. In 1951 Commander Harrison was selected for training in Advanced Science at Harvard University under sponsorship of the Office of Naval Research. This program led to the M. Eng. degree in 1952 and Ph.D. degree in Applied Physics in 1954. Commander Harrison is presently Electronics Officer on the Staff of Commander Operational Development Force. He is a member of several societies and associations including the Harvard Chapter of the Society of Sigma Xi.
Summary: The measurement of the magnetic field associated with a linearly or elliptically polarized electric field, using a small loop, or magnetic probe, is discussed. It is shown that in general a loop will not meas...
The effects on the ferromagnetism of a nitrogen defect in Cu-doped AlN with a Cu concentration of 2.77-8.33% have been investigated by first-principles. For Alω0.9723 Cuω0.0277 N, a global magnetic moment of 1.46μB...
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The design and construction of an automatic recording spectropolarimeter for measuring magnetooptical rotations (Faraday effect) in a magnetic field is described. The instrument has two opposed 5000 G magnetic fields ...
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The design and construction of an automatic recording spectropolarimeter for measuring magnetooptical rotations (Faraday effect) in a magnetic field is described. The instrument has two opposed 5000 G magnetic fields (one for solution and one for solvent) to give solute rotation directly as a function of wavelength (250–750 mμ) to a precision of ±0.001° in the visible and ±0.003° in the uv region of the spectrum. A description of the instrument performance and typical spectra is given.
The modes of Pacific decadal-scale variability (PDV), traditionally defined as statistical patterns of variance, reflect to first order the ocean's integration (i.e., reddening) of atmospheric forcing that ar...
The modes of Pacific decadal-scale variability (PDV), traditionally defined as statistical patterns of variance, reflect to first order the ocean's integration (i.e., reddening) of atmospheric forcing that arises from both a shift and a change in strength of the climatological (time-mean) atmospheric circulation. While these patterns concisely describe PDV, they do not distinguish among the key dynamical processes driving the evolution of PDV anomalies, including atmospheric and ocean teleconnections and coupled feedbacks with similar spatial structures that operate on different timescales. In this review, we synthesize past analysis using an empirical dynamical model constructed from monthly ocean surface anomalies drawn from several reanalysis products, showing that the PDV modes of variance result from two fundamental low-frequency dynamical eigenmodes: the North Pacific–central Pacific (NP-CP) and Kuroshio–Oyashio Extension (KOE) modes. Both eigenmodes highlight how two-way tropical–extratropical teleconnection dynamics are the primary mechanisms energizing and synchronizing the basin-scale footprint of PDV. While the NP-CP mode captures interannual- to decadal-scale variability, the KOE mode is linked to the basin-scale expression of PDV on decadal to multidecadal timescales, including contributions from the South Pacific.
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