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journal = {Oceanography},
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title = {Wind, {Waves}, and {Fronts}: {Frictional} {Effects} in a {Generalized} {Ekman} {Model}},
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year = {1994},
pages = {1--10}
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title = {A {Note} on the {Vertical} {Structure} of the {Eddy} {Exchange} {Coefficient} in the {Planetary} {Boundary} {Layer}},
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urldate = {2015-10-07},
journal = {Journal of the Atmospheric Sciences},
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pages = {1213--1215}
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title = {Oceanic wave-balanced surface fronts and filaments},
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urldate = {2015-10-06},
journal = {Journal of Fluid Mechanics},
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year = {2013},
pages = {464--490}
}
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title = {Langmuir turbulence in the ocean},
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pages = {1--30}
}
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title = {Submesoscale {Cold} {Filaments} in the {Gulf} {Stream}},
volume = {44},
issn = {0022-3670, 1520-0485},
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number = {10},
urldate = {2015-08-03},
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month = oct,
year = {2014},
pages = {2617--2643}
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title = {Diurnal cycle of rainfall and surface salinity in the {Western} {Pacific} {Warm} {Pool}},
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doi = {10.1029/1999GL010504},
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urldate = {2015-10-11},
journal = {Geophysical Research Letters},
author = {Cronin, Meghan F. and McPhaden, Michael J.},
month = dec,
year = {1999},
pages = {3465--3468}
}
@book{vallis_atmospheric_2006,
address = {Cambridge},
title = {Atmospheric and oceanic fluid dynamics: fundamentals and large-scale circulation},
isbn = {978-0-521-84969-2},
shorttitle = {Atmospheric and oceanic fluid dynamics},
publisher = {Cambridge University Press},
author = {Vallis, Geoffrey K.},
year = {2006},
keywords = {Fluid dynamics, Ocean-atmosphere interaction},
annote = {OCLC: ocm70671784}
}
@article{mooers_technique_1973,
title = {A technique for the cross spectrum analysis of pairs of complex-valued time series, with emphasis on properties of polarized components and rotational invariants},
volume = {20},
issn = {00117471},
url = {http://linkinghub.elsevier.com/retrieve/pii/0011747173900272},
doi = {10.1016/0011-7471(73)90027-2},
language = {en},
number = {12},
urldate = {2016-04-04},
journal = {Deep Sea Research and Oceanographic Abstracts},
author = {Mooers, Christopher N.K.},
month = dec,
year = {1973},
pages = {1129--1141}
}
@article{stuart-menteth_global_2003,
title = {A global study of diurnal warming using satellite-derived sea surface temperature},
volume = {108},
issn = {0148-0227},
url = {http://doi.wiley.com/10.1029/2002JC001534},
doi = {10.1029/2002JC001534},
language = {en},
number = {C5},
urldate = {2015-10-11},
journal = {Journal of Geophysical Research},
author = {Stuart-Menteth, Alice C.},
year = {2003}
}
@article{stommel_wind-drift_1960,
title = {Wind-drift near the equator},
volume = {6},
issn = {01466313},
url = {http://linkinghub.elsevier.com/retrieve/pii/0146631359900887},
doi = {10.1016/0146-6313(59)90088-7},
language = {en},
urldate = {2015-08-03},
journal = {Deep Sea Research (1953)},
author = {Stommel, Henry},
year = {1960},
pages = {298--302}
}
@article{thorpe_marginal_2009,
title = {Marginal {Instability}?},
volume = {39},
issn = {0022-3670, 1520-0485},
url = {http://journals.ametsoc.org/doi/abs/10.1175/2009JPO4153.1},
doi = {10.1175/2009JPO4153.1},
language = {en},
number = {9},
urldate = {2015-10-11},
journal = {Journal of Physical Oceanography},
author = {Thorpe, S. A. and Liu, Zhiyu},
month = sep,
year = {2009},
pages = {2373--2381}
}
@article{dewey_enhancement_1990,
title = {Enhancement of fronts by vertical mixing},
volume = {95},
issn = {0148-0227},
url = {http://doi.wiley.com/10.1029/JC095iC06p09433},
doi = {10.1029/JC095iC06p09433},
language = {en},
number = {C6},
urldate = {2015-08-03},
journal = {Journal of Geophysical Research},
author = {Dewey, Richard K. and Moum, James N.},
year = {1990},
pages = {9433}
}
@article{pawlowicz_classical_2002,
title = {Classical tidal harmonic analysis including error estimates in {MATLAB} using {T}\_TIDE},
volume = {28},
issn = {00983004},
url = {http://linkinghub.elsevier.com/retrieve/pii/S0098300402000134},
doi = {10.1016/S0098-3004(02)00013-4},
language = {en},
number = {8},
urldate = {2015-10-11},
journal = {Computers \& Geosciences},
author = {Pawlowicz, Rich and Beardsley, Bob and Lentz, Steve},
month = oct,
year = {2002},
pages = {929--937}
}
@article{fairall_bulk_2003,
title = {Bulk {Parameterization} of {Air}{\textendash}{Sea} {Fluxes}: {Updates} and {Verification} for the {COARE} {Algorithm}},
volume = {16},
issn = {0894-8755, 1520-0442},
shorttitle = {Bulk {Parameterization} of {Air}{\textendash}{Sea} {Fluxes}},
url = {http://journals.ametsoc.org/doi/abs/10.1175/1520-0442%282003%29016%3C0571%3ABPOASF%3E2.0.CO%3B2},
doi = {10.1175/1520-0442(2003)016<0571:BPOASF>2.0.CO;2},
language = {en},
number = {4},
urldate = {2015-08-03},
journal = {Journal of Climate},
author = {Fairall, C. W. and Bradley, E. F. and Hare, J. E. and Grachev, A. A. and Edson, J. B.},
month = feb,
year = {2003},
pages = {571--591}
}
@book{wilcox_fundamentals_2010,
title = {Fundamentals of modern statistical methods: {Substantially} improving power and accuracy},
shorttitle = {Fundamentals of modern statistical methods},
url = {https://books.google.com/books?hl=en&lr=&id=uUNGzhdxk0kC&oi=fnd&pg=PR7&dq=Fundamentals+of+Modern+Statistical+Methods:+Substantially+Improving+Power+and+Accuracy&ots=ZTkXEghIhG&sig=_U7NFBIp4L55WW40VXRn73PFahc},
urldate = {2015-10-11},
publisher = {Springer Science \& Business Media},
author = {Wilcox, Rand R.},
year = {2010}
}
@article{tan_approximate_2001,
title = {An {Approximate} {Analytical} {Solution} {For} {The} {Baroclinic} {And} {Variable} {Eddy} {Diffusivity} {Semi}-{Geostrophic} {Ekman} {Boundary} {Layer}},
volume = {98},
issn = {0006-8314, 1573-1472},
url = {http://link.springer.com/article/10.1023/A%3A1018708726112},
doi = {10.1023/A:1018708726112},
abstract = {The WKB method has been used to develop an approximate solutionof the semi-geostrophic Ekman boundary layer with height-dependenteddy viscosity and a baroclinic pressure field. The approximate solutionretains the same simple form as the classical Ekman solution. Behavioursof the approximate solution are discussed for different eddy viscosityand the pressure systems. These features show that wind structure inthe semi-geostrophic Ekman boundary layer depends on the interactionbetween the inertial acceleration, variable eddy viscosity and baroclinicpressure gradient. Anticyclonic shear has an acceleration effect on theair motion in the boundary layer, while cyclonic shear has a decelerationeffect. Decreasing pressure gradient with height results in a super-geostrophicpeak in the wind speed profile, however the increasing pressure gradient withheight may remove the peak. Anticyclonic shear and decreasing the variableeddy viscosity with height has an enhanced effect on the peak. Variable eddy viscosity and inertial acceleration has an important role in thedivergence and vorticity in the boundary layer and the vertical motion at the top of the boundary layer that is called Ekman pumping. Compared to the constanteddy viscosity case, the variable eddy diffusivity reduces the absolute value ofEkman pumping, especially in the case of eddy viscosity initially increasing with height. The difference in the Ekman pumping produced by different eddy diffusivity assumptions is intensified in anticyclonic flow and reduced in cyclonic flow.},
language = {en},
number = {3},
urldate = {2015-08-03},
journal = {Boundary-Layer Meteorology},
author = {Tan, Zhe-Min},
month = mar,
year = {2001},
keywords = {Atmospheric Protection/Air Quality Control/Air Pollution, Baroclinity, Boundary-layer wind, Ekman pumping, emi-geostrophic dynamics, Meteorology/Climatology, Variable eddy viscosity},
pages = {361--385}
}
@article{chu_ekman_2015,
title = {Ekman {Spiral} in a {Horizontally} {Inhomogeneous} {Ocean} with {Varying} {Eddy} {Viscosity}},
issn = {0033-4553, 1420-9136},
url = {http://link.springer.com/10.1007/s00024-015-1063-4},
doi = {10.1007/s00024-015-1063-4},
language = {en},
urldate = {2015-08-24},
journal = {Pure and Applied Geophysics},
author = {Chu, Peter C.},
month = mar,
year = {2015}
}
@article{kawai_diurnal_2007,
title = {Diurnal sea surface temperature variation and its impact on the atmosphere and ocean: {A} review},
volume = {63},
issn = {0916-8370, 1573-868X},
shorttitle = {Diurnal sea surface temperature variation and its impact on the atmosphere and ocean},
url = {http://link.springer.com/10.1007/s10872-007-0063-0},
doi = {10.1007/s10872-007-0063-0},
language = {en},
number = {5},
urldate = {2015-11-07},
journal = {Journal of Oceanography},
author = {Kawai, Yoshimi and Wada, Akiyoshi},
month = oct,
year = {2007},
pages = {721--744}
}
@article{wijffels_direct_1994,
title = {Direct {Observations} of the {Ekman} {Balance} at 10{\textdegree}{N} in the {Pacific}},
volume = {24},
issn = {0022-3670, 1520-0485},
url = {http://journals.ametsoc.org/doi/abs/10.1175/1520-0485%281994%29024%3C1666%3ADOOTEB%3E2.0.CO%3B2},
doi = {10.1175/1520-0485(1994)024<1666:DOOTEB>2.0.CO;2},
language = {en},
number = {7},
urldate = {2015-08-03},
journal = {Journal of Physical Oceanography},
author = {Wijffels, Susan and Firing, Eric and Bryden, Harry},
month = jul,
year = {1994},
pages = {1666--1679}
}
@article{chereskin_direct_1995,
title = {Direct evidence for an {Ekman} balance in the {California} {Current}},
volume = {100},
issn = {0148-0227},
url = {http://doi.wiley.com/10.1029/95JC02182},
doi = {10.1029/95JC02182},
language = {en},
number = {C9},
urldate = {2015-08-03},
journal = {Journal of Geophysical Research},
author = {Chereskin, T. K.},
year = {1995},
pages = {18261}
}
@article{caldwell_laboratory_1972,
title = {A laboratory study of the turbulent {Ekman} layer},
volume = {3},
issn = {0016-7991},
url = {http://www.tandfonline.com/doi/abs/10.1080/03091927208236078},
doi = {10.1080/03091927208236078},
language = {en},
number = {1},
urldate = {2015-08-03},
journal = {Geophysical Fluid Dynamics},
author = {Caldwell, D. R. and Van Atta, C. W. and Helland, K. N.},
month = jan,
year = {1972},
pages = {125--160}
}
@article{foltz_abrupt_2010,
title = {Abrupt equatorial wave-induced cooling of the {Atlantic} cold tongue in 2009},
volume = {37},
issn = {00948276},
url = {http://doi.wiley.com/10.1029/2010GL045522},
doi = {10.1029/2010GL045522},
language = {en},
number = {24},
urldate = {2015-10-11},
journal = {Geophysical Research Letters},
author = {Foltz, Gregory R. and McPhaden, Michael J.},
month = dec,
year = {2010},
pages = {n/a--n/a}
}
@article{schneider_sensitivity_1994,
title = {Sensitivity of the {Surface} {Equatorial} {Ocean} to the {Parameterization} of {Vertical} {Mixing}},
volume = {24},
issn = {0022-3670, 1520-0485},
doi = {10.1175/1520-0485(1994)024<1623:SOTSEO>2.0.CO;2},
language = {en},
number = {7},
urldate = {2015-10-11},
journal = {Journal of Physical Oceanography},
author = {Schneider, Niklas and M{\"u}ller, Peter},
month = jul,
year = {1994},
pages = {1623--1640}
}
@article{bunin_[influence_1975,
title = {[{The} influence of isoglaucon on the hydrodynamics and haemodynamics of the eye (author's transl)]},
volume = {167},
issn = {0023-2165},
abstract = {By animal experiments and clinically we could prove that isoglaucon instillation caused the decrease in IOP due to both increase in outflow and reduction of humor secretion; the IOP decrease and changes in hydrodynamics being manifested more markedly in the fellow-eye. As reoophthalmography demonstrated "Isoglaucon" produced lumen narrowing in the anterior portion of the uveal tract. "Isoglaucon" was prescribed to 20 patients having open-angle-glaucoma, Two hours after instillation the 23 decreased in 26 eyes (of 28) by 9.3 +/- 1.0 mm Hg. When prescribed regularly "Isoglaucon" raised the outflow facility coefficient from 0.10 +/- 0.01 to 0.20 +/-0.02. The secretion decreased from 2.0 +/- 0.2 to 0.9 +/- 0.15. Thus, IOP decrease after "Isoglaucon" is accounted for by both improved outflow and reduction of aqueous humor secretion. The "isoglucon" instillation produced a rather moderate decrease in the total arterial pressure, though no expected parallelism in arterial and intraocular pressure was marked.},
language = {ger},
number = {4},
journal = {Klinische Monatsbl{\"a}tter F{\"u}r Augenheilkunde},
author = {Bunin, A. J. and Jakovlev, A. A. and Jermakova, V. N. and Konde, L. A.},
month = oct,
year = {1975},
pmid = {1573},
keywords = {Animals, Aqueous Humor, Blood Pressure, Clonidine, Glaucoma, Hemodynamics, Humans, Hydrogen-Ion Concentration, Intraocular Pressure, Ophthalmic Artery, Ophthalmic Solutions, Rabbits},
pages = {542--549}
}
@article{schudlich_observations_1998,
title = {Observations of {Seasonal} {Variation} in the {Ekman} {Layer}},
volume = {28},
issn = {0022-3670, 1520-0485},
url = {http://journals.ametsoc.org/doi/abs/10.1175/1520-0485%281998%29028%3C1187%3AOOSVIT%3E2.0.CO%3B2},
doi = {10.1175/1520-0485(1998)028<1187:OOSVIT>2.0.CO;2},
language = {en},
number = {6},
urldate = {2015-08-03},
journal = {Journal of Physical Oceanography},
author = {Schudlich, Rebecca R. and Price, James F.},
month = jun,
year = {1998},
pages = {1187--1204}
}
@article{fairall_bulk_2003-1,
title = {Bulk {Parameterization} of {Air}{\textendash}{Sea} {Fluxes}: {Updates} and {Verification} for the {COARE} {Algorithm}},
volume = {16},
issn = {0894-8755, 1520-0442},
shorttitle = {Bulk {Parameterization} of {Air}{\textendash}{Sea} {Fluxes}},
doi = {10.1175/1520-0442(2003)016<0571:BPOASF>2.0.CO;2},
language = {en},
number = {4},
urldate = {2015-10-11},
journal = {Journal of Climate},
author = {Fairall, C. W. and Bradley, E. F. and Hare, J. E. and Grachev, A. A. and Edson, J. B.},
month = feb,
year = {2003},
pages = {571--591}
}
@book{temme_special_1996,
address = {New York},
title = {Special functions: an introduction to the classical functions of mathematical physics},
isbn = {978-0-471-11313-3},
shorttitle = {Special functions},
publisher = {Wiley},
author = {Temme, Nico M.},
year = {1996},
keywords = {Boundary value problems, Functions, Mathematical physics, Special}
}
@article{foltz_seasonal_2003,
title = {Seasonal mixed layer heat budget of the tropical {Atlantic} {Ocean}},
volume = {108},
issn = {0148-0227},
url = {http://doi.wiley.com/10.1029/2002JC001584},
doi = {10.1029/2002JC001584},
language = {en},
number = {C5},
urldate = {2015-08-03},
journal = {Journal of Geophysical Research},
author = {Foltz, Gregory R.},
year = {2003}
}
@article{smyth_local_1996,
title = {Local ocean response to a multiphase westerly wind burst: 1. {Dynamic} response},
volume = {101},
issn = {0148-0227},
shorttitle = {Local ocean response to a multiphase westerly wind burst},
doi = {10.1029/96JC02005},
language = {en},
number = {C10},
urldate = {2015-10-11},
journal = {Journal of Geophysical Research},
author = {Smyth, W. D. and Hebert, D. and Moum, J. N.},
year = {1996},
pages = {22495}
}
@book{noauthor_notitle_nodate,
url = {about:blank},
urldate = {2016-07-02}
}
@article{brainerd_surface_1995,
title = {Surface mixed and mixing layer depths},
volume = {42},
issn = {09670637},
url = {http://linkinghub.elsevier.com/retrieve/pii/096706379500068H},
doi = {10.1016/0967-0637(95)00068-H},
language = {en},
number = {9},
urldate = {2015-10-11},
journal = {Deep Sea Research Part I: Oceanographic Research Papers},
author = {Brainerd, Keith E. and Gregg, Michael C.},
month = sep,
year = {1995},
pages = {1521--1543}
}
@article{pollard_vorticity_1992,
title = {Vorticity and {Vertical} {Circulation} at an {Ocean} {Front}},
volume = {22},
issn = {0022-3670, 1520-0485},
url = {http://journals.ametsoc.org/doi/abs/10.1175/1520-0485%281992%29022%3C0609%3AVAVCAA%3E2.0.CO%3B2},
doi = {10.1175/1520-0485(1992)022<0609:VAVCAA>2.0.CO;2},
language = {en},
number = {6},
urldate = {2015-08-03},
journal = {Journal of Physical Oceanography},
author = {Pollard, R. T. and Regier, L. A.},
month = jun,
year = {1992},
pages = {609--625}
}
@article{thomas_destruction_2005,
title = {Destruction of {Potential} {Vorticity} by {Winds}},
volume = {35},
issn = {0022-3670, 1520-0485},
url = {http://journals.ametsoc.org/doi/abs/10.1175/JPO2830.1},
doi = {10.1175/JPO2830.1},
language = {en},
number = {12},
urldate = {2015-08-03},
journal = {Journal of Physical Oceanography},
author = {Thomas, Leif N.},
month = dec,
year = {2005},
pages = {2457--2466}
}
@book{gill_atmosphere-ocean_1982,
address = {New York},
series = {International geophysics series},
title = {Atmosphere-ocean dynamics},
isbn = {978-0-12-283522-3},
publisher = {Academic Press},
author = {Gill, Adrian E.},
year = {1982},
keywords = {Ocean-atmosphere interaction}
}
@article{berger_baroclinic_1998,
title = {The baroclinic, variable eddy viscosity {Ekman} layer},
volume = {87},
url = {http://link.springer.com/article/10.1023/A:1001076030166},
number = {3},
urldate = {2015-08-03},
journal = {Boundary-Layer Meteorology},
author = {Berger, Bradford W. and Grisogono, Branko},
year = {1998},
pages = {363--380}
}
@book{center_for_history_and_new_media_zotero_nodate-1,
title = {Zotero {Quick} {Start} {Guide}},
url = {http://zotero.org/support/quick_start_guide},
author = {{Center for History and New Media}}
}
@article{donlon_operational_2012,
series = {Advanced {Along} {Track} {Scanning} {Radiometer}({AATSR}) {Special} {Issue}},
title = {The {Operational} {Sea} {Surface} {Temperature} and {Sea} {Ice} {Analysis} ({OSTIA}) system},
volume = {116},
issn = {0034-4257},
url = {http://www.sciencedirect.com/science/article/pii/S0034425711002197},
doi = {10.1016/j.rse.2010.10.017},
abstract = {This paper describes a new Sea surface temperature (SST) analysis that is produced with global coverage on a daily basis at the Met Office called the Operational SST and Sea Ice Analysis (OSTIA) system. OSTIA uses satellite SST data provided by international agencies via the Group for High Resolution SST (GHRSST) Regional/Global Task Sharing (R/GTS) framework. GHRSST products include data from microwave and infrared satellite instruments with accompanying uncertainty estimates. The system also uses in situ SST data available over the Global Telecommunications System (GTS) and a sea-ice concentration product from the EUMETSAT Ocean and Sea Ice Satellite Applications Facility (OSI-SAF). The SST analysis is a multi-scale optimal interpolation that is designed for applications in numerical weather prediction and ocean forecasting systems. The background error covariance matrix is specified using ocean model data and the analysis uses correlation length scales of 10 km and 100 km. The OSTIA system produces a foundation SST estimate (SSTfnd, which is the SST free of diurnal variability) at an output grid resolution of 1/20{\textdegree} ({\textbackslash}textbackslashtextasciitilde 6 km) although the smallest analysis feature resolution is based on the correlation length scale of 10 km. All satellite SST data are adjusted for bias errors based on a combination of ENVISAT Advanced Along Track Scanning Radiometer (AATSR) SST data and in situ SST measurements from drifting buoys. Data are filtered (based on surface wind speed data) to remove diurnal variability and AATSR data are adjusted to represent the SST at the same depth as drifting buoy measurements (0.2{\textendash}1 m) before bias adjustments are made. Global coverage outputs are provided each day in GHRSST L4 netCDF format. A variety of secondary products are also provided including weekly and monthly mean data sets. OSTIA products are continuously monitored and validation/verification activities demonstrate that SST products have zero mean bias and an accuracy of {\textbackslash}textbackslashtextasciitilde 0.57 K compared to in situ measurements. OSTIA is now used operationally as a boundary condition for all weather forecast models at the Met Office and at European Centre for Medium-range Weather Forecasting (ECMWF). OSTIA is produced by the Met Office as part of the European Union Global Monitoring for Environment and Security (GMES) MyOcean project.},
urldate = {2015-08-03},
journal = {Remote Sensing of Environment},
author = {Donlon, Craig J. and Martin, Matthew and Stark, John and Roberts-Jones, Jonah and Fiedler, Emma and Wimmer, Werenfrid},
month = jan,
year = {2012},
keywords = {Sea ice, Sea surface temperature, SST},
pages = {140--158}
}
@article{thomas_intensification_2005,
title = {Intensification of {Ocean} {Fronts} by {Down}-{Front} {Winds}},
volume = {35},
issn = {0022-3670, 1520-0485},
url = {http://journals.ametsoc.org/doi/abs/10.1175/JPO2737.1},
doi = {10.1175/JPO2737.1},
language = {en},
number = {6},
urldate = {2015-08-03},
journal = {Journal of Physical Oceanography},
author = {Thomas, Leif N. and Lee, Craig M.},
month = jun,
year = {2005},
pages = {1086--1102}
}
@article{stern_interaction_1965,
title = {Interaction of a uniform wind stress with a geostrophic vortex},
volume = {12},
issn = {00117471},
url = {http://linkinghub.elsevier.com/retrieve/pii/0011747165900070},
doi = {10.1016/0011-7471(65)90007-0},
language = {en},
number = {3},
urldate = {2015-08-03},
journal = {Deep Sea Research and Oceanographic Abstracts},
author = {Stern, Melvin E.},
month = jun,
year = {1965},
pages = {355--367}
}
@incollection{boyer_world_2013,
address = {Silver Spring, MD},
title = {World {Ocean} {Database} 2013},
booktitle = {{NOAA} {Atlas} {NESDIS} 72},
publisher = {National Oceanic and Atmospheric Administration},
author = {Boyer, T.P.},
year = {2013}
}
@article{polton_role_2005,
title = {The role of wave-induced {Coriolis}-{Stokes} forcing on the wind-driven mixed layer},
volume = {35},
url = {http://journals.ametsoc.org/doi/abs/10.1175/JPO2701.1},
number = {4},
urldate = {2015-08-03},
journal = {Journal of Physical Oceanography},
author = {Polton, Jeff A. and Lewis, David M. and Belcher, Stephen E.},
year = {2005},
pages = {444--457}
}
@article{schmidtko_mimoc:_2013-1,
title = {{MIMOC}: {A} global monthly isopycnal upper-ocean climatology with mixed layers: {MIMOC}},
volume = {118},
issn = {21699275},
shorttitle = {{MIMOC}},
url = {http://doi.wiley.com/10.1002/jgrc.20122},
doi = {10.1002/jgrc.20122},
language = {en},
number = {4},
urldate = {2015-08-03},
journal = {Journal of Geophysical Research: Oceans},
author = {Schmidtko, Sunke and Johnson, Gregory C. and Lyman, John M.},
month = apr,
year = {2013},
pages = {1658--1672}
}
@article{smyth_diurnal_2013,
title = {Diurnal {Shear} {Instability}, the {Descent} of the {Surface} {Shear} {Layer}, and the {Deep} {Cycle} of {Equatorial} {Turbulence}},
volume = {43},
issn = {0022-3670, 1520-0485},
url = {http://journals.ametsoc.org/doi/abs/10.1175/JPO-D-13-089.1},
doi = {10.1175/JPO-D-13-089.1},
language = {en},
number = {11},
urldate = {2015-08-03},
journal = {Journal of Physical Oceanography},
author = {Smyth, W. D. and Moum, J. N. and Li, L. and Thorpe, S. A.},
month = nov,
year = {2013},
pages = {2432--2455}
}
@article{danabasoglu_diurnal_2006,
title = {Diurnal {Coupling} in the {Tropical} {Oceans} of {CCSM3}},
volume = {19},
issn = {0894-8755, 1520-0442},
url = {http://journals.ametsoc.org/doi/abs/10.1175/JCLI3739.1},
doi = {10.1175/JCLI3739.1},
language = {en},
number = {11},
urldate = {2015-10-11},
journal = {Journal of Climate},
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year = {2004},
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pmid = {10},
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@book{bender_advanced_1978,
address = {New York},
title = {Advanced mathematical methods for scientists and engineers},
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publisher = {Springer},
author = {Bender, Carl M. and Orszag, Steven A.},
year = {1978},
keywords = {Differential equations, Numerical solutions, Difference equations, Engineering mathematics, Mathematics, Science}