Example of Journal of Physical Oceanography format
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Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format
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Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format Example of Journal of Physical Oceanography format
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open access Open Access ISSN: 223670 e-ISSN: 15200485

Journal of Physical Oceanography — Template for authors

Categories Rank Trend in last 3 yrs
Oceanography #17 of 128 down down by 6 ranks
journal-quality-icon Journal quality:
High
calendar-icon Last 4 years overview: 687 Published Papers | 3778 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 03/07/2020
Insights & related journals
General info
Top papers
Popular templates
Get started guide
Why choose from SciSpace
FAQ

Journal Performance & Insights

  • Impact Factor
  • CiteRatio
  • SJR
  • SNIP

Impact factor determines the importance of a journal by taking a measure of frequency with which the average article in a journal has been cited in a particular year.

3.318

2% from 2018

Impact factor for Journal of Physical Oceanography from 2016 - 2019
Year Value
2019 3.318
2018 3.389
2017 3.086
2016 3.13
graph view Graph view
table view Table view

insights Insights

  • Impact factor of this journal has decreased by 2% in last year.
  • This journal’s impact factor is in the top 10 percentile category.

CiteRatio is a measure of average citations received per peer-reviewed paper published in the journal.

5.5

11% from 2019

CiteRatio for Journal of Physical Oceanography from 2016 - 2020
Year Value
2020 5.5
2019 6.2
2018 5.6
2017 5.6
2016 5.4
graph view Graph view
table view Table view

insights Insights

  • CiteRatio of this journal has decreased by 11% in last years.
  • This journal’s CiteRatio is in the top 10 percentile category.

SCImago Journal Rank (SJR) measures weighted citations received by the journal. Citation weighting depends on the categories and prestige of the citing journal.

1.706

26% from 2019

SJR for Journal of Physical Oceanography from 2016 - 2020
Year Value
2020 1.706
2019 2.292
2018 2.48
2017 2.461
2016 2.741
graph view Graph view
table view Table view

insights Insights

  • SJR of this journal has decreased by 26% in last years.
  • This journal’s SJR is in the top 10 percentile category.

Source Normalized Impact per Paper (SNIP) measures actual citations received relative to citations expected for the journal's category.

1.429

10% from 2019

SNIP for Journal of Physical Oceanography from 2016 - 2020
Year Value
2020 1.429
2019 1.588
2018 1.37
2017 1.289
2016 1.371
graph view Graph view
table view Table view

insights Insights

  • SNIP of this journal has decreased by 10% in last years.
  • This journal’s SNIP is in the top 10 percentile category.

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CiteRatio: 5.0 | SJR: 1.558 | SNIP: 1.437
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CiteRatio: 5.0 | SJR: 1.13 | SNIP: 1.266
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CiteRatio: 3.6 | SJR: 0.761 | SNIP: 1.013

Journal of Physical Oceanography

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American Meteorological Society

Journal of Physical Oceanography

Research related to the physics of the ocean and to processes operating at its boundaries. Observational, theoretical, and modeling studies are all welcome, especially those that focus on elucidating specific physical processes. Papers that investigate interactions with other ...... Read More

Oceanography

Earth and Planetary Sciences

i
Last updated on
02 Jul 2020
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ISSN
0022-3670
i
Impact Factor
High - 1.379
i
Acceptance Rate
Not provided
i
Frequency
Not provided
i
Open Access
No
i
Sherpa RoMEO Archiving Policy
Yellow faq
i
Plagiarism Check
Available via Turnitin
i
Endnote Style
Download Available
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Bibliography Name
numbered
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Citation Type
Author Year
(Blonder et al. 1982)
i
Bibliography Example
Blonder, G. E., M. Tinkham, and T. M. Klapwijk, 1982: Transition from metallic to tunneling regimes in superconducting microconstrictions: Excess current, charge imbalance, and supercurrent conversion. Phys. Rev. B, 25 (7), 4515–4532, URL 10.1103/PhysRevB.25.4515.

Top papers written in this journal

Isopycnal mixing in ocean circulation models
Peter R. Gent1, James C. McWilliams1

Abstract:

A subgrid-scale form for mesoscale eddy mixing on isopycnal surfaces is proposed for use in non-eddy-resolving ocean circulation models. The mixing is applied in isopycnal coordinates to isopycnal layer thickness, or inverse density gradient, as well as to passive scalars, temperature and salinity. The transformation of these... A subgrid-scale form for mesoscale eddy mixing on isopycnal surfaces is proposed for use in non-eddy-resolving ocean circulation models. The mixing is applied in isopycnal coordinates to isopycnal layer thickness, or inverse density gradient, as well as to passive scalars, temperature and salinity. The transformation of these mixing forms to physical coordinates is also presented. read more read less

Topics:

Isopycnal (71%)71% related to the paper, Mixing (physics) (55%)55% related to the paper, Ocean general circulation model (55%)55% related to the paper, Parallel Ocean Program (54%)54% related to the paper, Temperature salinity diagrams (52%)52% related to the paper
2,869 Citations
Open Ocean Momentum Flux Measurements in Moderate to Strong Winds
W. G. Large1, Stephen Pond1

Abstract:

Measurements of the momentum flux were made by the Reynolds flux and dissipation methods on a deep water stable tower operated by the Bedford Institute of Oceanography, A modified Gill propeller-vane anemometer was used to measure the velocity. Drag coefficients from 196 Reynolds flux measurements agree well with those report... Measurements of the momentum flux were made by the Reynolds flux and dissipation methods on a deep water stable tower operated by the Bedford Institute of Oceanography, A modified Gill propeller-vane anemometer was used to measure the velocity. Drag coefficients from 196 Reynolds flux measurements agree well with those reported in Smith (1980) based on independent observations at the same site. Based on 192 runs, a comparison of the dissipation and Reynolds flux results shows excellent agreement on average, for wind speeds from 4 to 20 m s−1. The much more extensive dissipation data set (1086 h from the tower and 505 h from the weathership PAPA, CCGS Quadra) was used to investigate the dependence of the drag coefficient on wind speed, fetch and stability. The drag coefficient reduced to 10 m height and neutral conditions (CDN), is independent of stability and fetch (for fetch/height ≳800) but increases with wind speed above 10 m s−1. Some time series of the momentum flux and drag coefficient are ... read more read less

Topics:

Drag coefficient (63%)63% related to the paper, Fetch (57%)57% related to the paper, Wind speed (54%)54% related to the paper, Flux (53%)53% related to the paper, Anemometer (52%)52% related to the paper
2,480 Citations
Normal Monthly Wind Stress Over the World Ocean with Error Estimates
Sol Hellerman1, Mel Rosenstein1

Abstract:

Over 35 million surface observations covering the world ocean from 1870–1976 have been processed for the purpose of calculating monthly normals and standard errors of the eastward and northward components of the wind stress and work done by the winds in the lower 10 m of the atmosphere. The fields are intended to serve as bou... Over 35 million surface observations covering the world ocean from 1870–1976 have been processed for the purpose of calculating monthly normals and standard errors of the eastward and northward components of the wind stress and work done by the winds in the lower 10 m of the atmosphere. The fields are intended to serve as boundary conditions for models of the ocean circulation. Wind and air-minus-sea temperatures are calculated in a form suitable for determining stress by any bulk aerodynamics model in which the drag coefficient can be represented by six or less coefficients of a second-degree polynomial in wind speed and stability. The particular case of the wind speed and stability dependent drag coefficient discussed by Bunker is selected for analysis. January and July charts of wind stress, curl of the wind stress, mass transport stream-function, divergence of the Ekman transport and the rate of mechanical energy transfer are illustrated and discussed. read more read less

Topics:

Wind stress (69%)69% related to the paper, Wind shear (67%)67% related to the paper, Wind gradient (66%)66% related to the paper, Wind profile power law (66%)66% related to the paper, Wind speed (63%)63% related to the paper
1,857 Citations
A Dynamic Thermodynamic Sea Ice Model
William D. Hibler1

Abstract:

A numerical model for the simulation of sea ice circulation and thickness over a seasonal cycle is presented. This model is used to investigate the effects of ice dynamics on Arctic ice thickness and air-sea heat flux characteristics by carrying out several numerical simulations over the entire Arctic Ocean region. The essent... A numerical model for the simulation of sea ice circulation and thickness over a seasonal cycle is presented. This model is used to investigate the effects of ice dynamics on Arctic ice thickness and air-sea heat flux characteristics by carrying out several numerical simulations over the entire Arctic Ocean region. The essential idea in the model is to couple the dynamics to the ice thickness characteristics by allowing the ice interaction to become stronger as the ice becomes thicker and/or contains a lower areas percentage of thin ice. The dynamics in turn causes high oceanic heat losses in regions of ice divergence and reduced heat losses in regions of convergence. TO model these effects consistently the ice is considered to interact in a plastic manner with the plastic strength chosen to depend on the ice thickness and concentration. The thickness and concentration, in turn, evolve according to continuity equations which include changes in ice mass and percent of open water due to advection, ... read more read less

Topics:

Sea ice thickness (80%)80% related to the paper, Arctic ice pack (80%)80% related to the paper, Sea ice (79%)79% related to the paper, Ice divide (78%)78% related to the paper, Sea ice growth processes (77%)77% related to the paper
1,834 Citations
Estimates of the Local Rate of Vertical Diffusion from Dissipation Measurements
Thomas R. Osborn1

Abstract:

Scaling of the turbulent energy equation suggests the balance of terms in the ocean is between turbulent production, dissipation and the loss to buoyancy. In this paper two models for the source of oceanic turbulence are considered; namely, production by the Reynolds stress working against a time variable mean shear, and the ... Scaling of the turbulent energy equation suggests the balance of terms in the ocean is between turbulent production, dissipation and the loss to buoyancy. In this paper two models for the source of oceanic turbulence are considered; namely, production by the Reynolds stress working against a time variable mean shear, and the gravitational collapse of Kelvin-Helmholtz instabilities. Both of these shear instabilities are believed to be important in the ocean. Using values for the critical flux Richardson number and the measurements from studies of Kelvin-Helmholtz instabilities, the efficiency of turbulent mixing is shown to be comparable for the two models. Therefore, a general relationship between the dissipation rate and the buoyancy flux due to the small-scale turbulent velocity fluctuations is derived. The result is expressed as an upper bound on the value of the turbulent eddy coefficient for mass Kρ ⩽ 0.2ϵ/N2. Values of Kρ are calculated from recent oceanic measurements of energy dissipation... read more read less

Topics:

Richardson number (57%)57% related to the paper, Turbulence (55%)55% related to the paper, Reynolds stress (54%)54% related to the paper, Buoyancy (53%)53% related to the paper, Dissipation (51%)51% related to the paper
1,722 Citations
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Journal of Physical Oceanography format uses numbered citation style.

Automatically format and order your citations and bibliography in a click.

SciSpace allows imports from all reference managers like Mendeley, Zotero, Endnote, Google Scholar etc.

Frequently asked questions

Absolutely not! With our tool, you can freely write without having to focus on LaTeX. You can write your entire paper as per the Journal of Physical Oceanography guidelines and autoformat it.

Yes. The template is fully compliant as per the guidelines of this journal. Our experts at SciSpace ensure that. Also, if there's any update in the journal format guidelines, we take care of it and include that in our algorithm.

Sure. We support all the top citation styles like APA style, MLA style, Vancouver style, Harvard style, Chicago style, etc. For example, in case of this journal, when you write your paper and hit autoformat, it will automatically update your article as per the Journal of Physical Oceanography citation style.

You can avail our Free Trial for 7 days. I'm sure you'll find our features very helpful. Plus, it's quite inexpensive.

Yup. You can choose the right template, copy-paste the contents from the word doc and click on auto-format. You'll have a publish-ready paper that you can download at the end.

A matter of seconds. Besides that, our intuitive editor saves a load of your time in writing and formating your manuscript.

One little Google search can get you the Word template for any journal. However, why do you need a Word template when you can write your entire manuscript on SciSpace, autoformat it as per Journal of Physical Oceanography's guidelines and download the same in Word, PDF and LaTeX formats? Try us out!.

Absolutely! You can do it using our intuitive editor. It's very easy. If you need help, you can always contact our support team.

SciSpace is an online tool for now. We'll soon release a desktop version. You can also request (or upvote) any feature that you think might be helpful for you and the research community in the feature request section once you sign-up with us.

Sure. You can request any template and we'll have it up and running within a matter of 3 working days. You can find the request box in the Journal Gallery on the right sidebar under the heading, "Couldn't find the format you were looking for?".

After you have written and autoformatted your paper, you can download it in multiple formats, viz., PDF, Docx and LaTeX.

To be honest, the answer is NO. The impact factor is one of the many elements that determine the quality of a journal. Few of those factors the review board, rejection rates, frequency of inclusion in indexes, Eigenfactor, etc. You must assess all the factors and then take the final call.

SHERPA/RoMEO Database

We have extracted this data from Sherpa Romeo to help our researchers understand the access level of this journal. The following table indicates the level of access a journal has as per Sherpa Romeo Archiving Policy.

RoMEO Colour Archiving policy
Green Can archive pre-print and post-print or publisher's version/PDF
Blue Can archive post-print (ie final draft post-refereeing) or publisher's version/PDF
Yellow Can archive pre-print (ie pre-refereeing)
White Archiving not formally supported
FYI:
  1. Pre-prints as being the version of the paper before peer review and
  2. Post-prints as being the version of the paper after peer-review, with revisions having been made.

The 5 most common citation types in order of usage are:.

S. No. Citation Style Type
1. Author Year
2. Numbered
3. Numbered (Superscripted)
4. Author Year (Cited Pages)
5. Footnote

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After uploading your paper on SciSpace, you would see a button to request a journal submission service for Journal of Physical Oceanography.

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Yes. SciSpace provides this functionality.

After signing up, you would need to import your existing references from Word or .bib file.

SciSpace would allow download of your references in Journal of Physical Oceanography Endnote style, according to american-meteorological-society guidelines.

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