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Institution

Naval Postgraduate School

EducationMonterey, California, United States
About: Naval Postgraduate School is a education organization based out in Monterey, California, United States. It is known for research contribution in the topics: Tropical cyclone & Nonlinear system. The organization has 5246 authors who have published 11614 publications receiving 298300 citations. The organization is also known as: NPS & U.S. Naval Postgraduate School.


Papers
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Journal ArticleDOI
TL;DR: It is concluded that the anisotropic coefficient influences both the long-term beam spread and the scintillation index by the factor ς(2-α).
Abstract: A wealth of experimental data has shown that atmospheric turbulence can be anisotropic; in this case, a Kolmogorov spectrum does not describe well the atmospheric turbulence statistics. In this paper, we show a quantitative analysis of anisotropic turbulence by using a non-Kolmogorov power spectrum with an anisotropic coefficient. The spectrum we use does not include the inner and outer scales, it is valid only inside the inertial subrange, and it has a power-law slope that can be different from a Kolmogorov one. Using this power spectrum, in the weak turbulence condition, we analyze the impact of the power-law variations α on the long-term beam spread and scintillation index for several anisotropic coefficient values ς. We consider only horizontal propagation across the turbulence cells, assuming circular symmetry is maintained on the orthogonal plane to the propagation direction. We conclude that the anisotropic coefficient influences both the long-term beam spread and the scintillation index by the factor ς2−α.

124 citations

Journal ArticleDOI
TL;DR: In this article, large-scale changes in the circulation of sea ice and the upper layers of the arctic ocean have been reported during the last decade using a regional coupled ice-ocean model, and the authors hypothesize that these changes are inresponsetoevenlargerscale atmo-spheric variability in the Northern Hemisphere that can be denedaseithertheArcticOscillationortheNorthAtlantic Oscillation.
Abstract: Dramatic changes in the circulation of sea ice andtheupperlayersoftheArcticOceanhavebeenreported during the last decade. Similar variability is modeled using a regional, coupled ice-ocean model. Realistic atmospheric forcingeldsfor1979-93 aretheonlyinterannualsignalpre- scribed in the model. Our results show large-scale changes inseaiceandoceanicconditionswhencomparingresultsfor the late 1970s / early 1980s and the 1990s. We hypothesize thatthesechangesareinresponsetoevenlargerscaleatmo- spheric variability in the Northern Hemisphere that can be denedaseithertheArcticOscillationortheNorthAtlantic Oscillation. Agreement between the direction and scale of change in the model and observations, in the absence of in- terannual forcing from the global ocean thermohaline circu- lation, suggests that the atmospheric variability by itself is sucienttoproducebasin-scalechangesintheArcticOcean and sea ice system.

124 citations

Journal ArticleDOI

124 citations

Journal ArticleDOI
TL;DR: In this paper, surface, airborne, and satellite measurements over the eastern Pacific Ocean off the coast of California during the period between 2005 and 2007 are used to explore the relationship between ocean chlorophyll, aerosol, and marine clouds.
Abstract: Surface, airborne, and satellite measurements over the eastern Pacific Ocean off the coast of California during the period between 2005 and 2007 are used to explore the relationship between ocean chlorophyll a, aerosol, and marine clouds. Periods of enhanced chlorophyll a and wind speed are coincident with increases in particulate diethylamine and methanesulfonate concentrations. The measurements indicate that amines are a source of secondary organic aerosol in the marine atmosphere. Subsaturated aerosol hygroscopic growth measurements indicate that the organic component during periods of high chlorophyll a and wind speed exhibit considerable water uptake ability. Increased average cloud condensation nucleus (CCN) activity during periods of increased chlorophyll a levels likely results from both size distribution and aerosol composition changes. The available data over the period of measurements indicate that the cloud microphysical response, as represented by either cloud droplet number concentration or cloud droplet effective radius, is likely influenced by a combination of atmospheric dynamics and aerosol perturbations during periods of high chlorophyll a concentrations.

124 citations


Authors

Showing all 5313 results

NameH-indexPapersCitations
Mingwei Chen10853651351
O. C. Zienkiewicz10745571204
Richard P. Bagozzi104347103667
Denise M. Rousseau8421850176
John Walsh8175625364
Ming C. Lin7637023466
Steven J. Ghan7520725650
Hui Zhang7520027206
Clare E. Collins7156021443
Christopher W. Fairall7129319756
Michael T. Montgomery6825814231
Tim Li6738316370
Thomas M. Antonsen6588817583
Nadia Magnenat-Thalmann6552114850
Johnny C. L. Chan6126114886
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Performance
Metrics
No. of papers from the Institution in previous years
YearPapers
202331
2022151
2021321
2020382
2019352
2018362