Satellite Oceanography and Meteorology

Editor-in-ChiefSheng, Jinyu

ISSN: 2424-9505 (Online)

ISSN: 2424-8959 (Print)

Journal Abbreviation: Satell Oceanogr Meteorol

Publication Frequency: bi-annual

Article Processing Charges (APC): Click here for more details

Publishing Model: Open Access

Journal no: 10P

About the Journal

The Satellite Oceanography and Meteorology (SOM) was launched in 2016, in response to the growing use of remotely sensed satellite data in understanding and identifying important processes and phenomena occurring in the atmosphere and ocean. The SOM provides space for oceanographers, meteorologists, hydrologists and climatologists to publish their research papers on theory, science, technology and applications of satellite remote sensing data of the ocean, atmosphere and climate.

Recently Published Articles

Articles

Xiaoming Zhai
46 Views, 79 PDF Downloads
The annual cycle of surface eddy kinetic energy (EKE) and its influence on eddy momentum fluxes are investigated using an updated record of satellite altimeter data. It is found that there is a phase difference between the annual cycles of EKE in the western boundary current regions and EKE in the interior of the subtropical gyres, suggesting that different mechanisms may be at work in different parts of the subtropical gyres. The annual cycles of EKE averaged in the two hemispheres are found to be of similar magnitude but in opposite phase. As a result, the globally-averaged EKE shows little seasonal variability. The longer record of altimeter data used in this study has brought out a clearer and simpler picture of eddy momentum fluxes in the Gulf Stream and Kuroshio Extension. Considerable seasonal variations in eddy momentum fluxes are found in the western boundary current regions, which potentially play an important role in modulating the strength of the western boundary currents and their associated recirculation gyres on the seasonal time scale.
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Articles

Guang Jun Zhang, Mingcheng Wang
40 Views, 23 PDF Downloads

How high convective clouds can go is of great importance to climate. Cloud ice and liquid water that detrain near the top of convective cores are important for the formation of anvil clouds and thus impact cloud radiative forcing and the Earth’s radiation budget. This study uses CloudSat observations to evaluate convective cloud top heights in the National Center for Atmospheric Research (NCAR) Community Atmosphere Model (CAM5). Results show that convective cloud top heights in the tropics are much lower than observed by CloudSat, by more than 2 km on average. Temperature and moisture anomalies from climatological means are composited for convective clouds of different heights for both observations and model simulation. It is found that convective environment is warmer and moister, and the anomalies are larger for clouds of higher tops. For a given convective cloud top height, the corresponding atmosphere in CAM5 is more convectively unstable than what the CloudSat observations indicate, suggesting that there is too much entrainment into convective clouds in the model.

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Editorial

Jinyu Sheng
53 Views, 30 PDF Downloads

The journal of Satellite Oceanography and Meteorology (SOM) was launched in 2016 for inspiring and disseminating research papers on theory, science, technology and applications of satellite remote sensing data of the ocean, atmosphere and climate. We welcome research papers in areas of (a) original research results from satellite observations of the regional and global ocean and atmosphere, (b) calibration/validation and research related to future satellite missions, and (c) new satellite-derived products and climate records constructed from satellite observations. We also welcome high-quality research papers in broad research areas including but not limiting to (i) oceanography and marine science; (ii) meteorology and atmospheric science; (iii) air-sea, physical-biological and physical-chemical interactions, and (iv) studies of the Earth’s climate system.

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Articles

Tao Xie, Li Zhao, William Perrie, He Fang
18 Views, 25 PDF Downloads

Climate change, increasing activities in areas like offshore oil and gas exploration, marine transport, eco-tourism, in additional to the usual activities of northerners resident are leading to reductions in sea ice. Therefore, there is an urgent need for improvement in the sea ice detection in polar areas. Starting from the mechanism of electromagnetic scattering, based on an empirical dielectric constant model, we apply EM multi-reflection and transmission formulas for coefficients between the air-ice interface and sea water-ice interface to develop a model for estimating the capability of detection of sea ice and ice thickness based on a pulse radar system, synthetic aperture radar (SAR). Although the dielectric constant of sea ice is less than that of sea water, this model can provide a rational methodology as the normalized radar cross section (NRCS) of sea ice is larger than that of sea water due to multiple reflections. The numerical simulations of this model showed that the convergence rate is rapid. With 3 or 4 reflections and transmissions (depending on temperature, salinity, and dielectric constants of sea ice and water), truncation errors can be satisfied using theoretical considerations and practical applications. The model is applied to estimate the capability of SAR to discriminate ice from water. The numerical results suggested that the model ability to measure ice thickness decreases with increasing radar incident angles and increases with increasing radar pulse width. Reflection and transmission coefficients decrease monotonically with ice thickness and are saturated for ice thicknesses above a certain critical value which depends on SAR incidence angle, frequency and dielectric constants of sea ice. The capability to detect ice thickness for given different bands of pulse radar widths can be estimated with this model.

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Articles

Qingtao Song, Zhaohui Wang
86 Views, 64 PDF Downloads
Motivated by the shortcomings of radio frequency interferences (RFI) associated with the spaceborne L-band radiometers near the Northwest Pacific and previous study near the Amazon plume, this study presents a sea surface salinity (SSS) retrieval algorithm from the microwave radiometer onboard the HY-2A satellite. The SSS signal is improved by differentiating the reflectance between the C and X band. A reflectance calibration method is proposed by using a combination of radiative transfer model (RTM) and the Klein-Swift emissivity model. Evaluations of the retrieved SSS from the HY-2A satellite indicate that the root mean square error (RMSE) is about 0.35 psu on 0.5 degree grid spacing and monthly time scale which is comparable to the accuracy of SMOS and Aquarius-SAC/D satellites.
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Articles

Hui Yang, Yuanfa Gong, Gui-Ying Yang
68 Views, 204 PDF Downloads
The relationship between tropical convective activities and meridional (north-south) migration of the East Asian jet stream (EAJS) in winter (December-February) is investigated for improving our knowledge of processes affecting the meridional migration of the EAJS. The monthly mean fields of outgoing longwave radiation (OLR) produced by NCAR and monthly atmospheric circulations produced by the NCEP/NCAR are used in this study. For 31 winter seasons between 1980 and 2011, the meridional migration of the winter EAJS is found to be strongly correlated with the present and preceding conditions of tropical convection over Indonesia. The anomalies in the tropical convection over the region in the preceding autumn and even preceding summer are a very useful indicator for the abnormal meridional migration of the wintertime EAJS. When the tropical convection over Indonesia weakens (strengthens), the EAJS has an abnormal southward (northward) migration. The atmospheric circulation associated with the abnormal meridional migration of the EAJS features abnormal air temperatures over the EAJS and its south side. The center of abnormal air temperatures occurs over the region south of the Yangtze River. Abnormal air pressures generated by abnormal air temperatures lead to abnormal winds. In the case of weakened tropical convection (positive OLR anomaly) over Indonesia, ascending motion of air mass over Indonesia is reduced, and the strength of Hadley circulation is weakened over the meridional range of the western Pacific Ocean. Consequently, the high-level air mass to the south of the core of the EAJS abnormally ascends and cools and the nearly southerly divergent winds at high-altitudes weaken, leading to significant reduction of heat transport from tropics to the southern China, with negative anomalies of air temperatures in the EAJS and its south side. The above processes increase thermal winds to the south of the Yangtze River and enhance the high-level westerly winds. To the north of the Yangtze River, both thermal winds and the high-level westerly winds are reduced. As a result, the EAJS has an abnormal south migration. In the case of enhanced tropical convection (negative OLR anomaly) over Indonesia, the opposite happens, in which Hadley circulation strengthens, the air mass to the south of the core of the EAJS abnormally descends and warms, heat transport increases from tropics to the southern China with positive air temperatures anomalies over the EAJS and its south side, and the EAJS has an abnormal northward migration.
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Articles

Xingrong Chen, Yi Cai, Fangli Qiao
69 Views, 66 PDF Downloads

The physical decomposition method suggested by Qian (2012) is used to examine the interannual variability of sea surface temperature (SST) and anomaly (SSTA) in the Indian Ocean (IO) for the period 1945.2003. The monthly mean SSTs taken from the global ocean reanalysis produced by the Simple Ocean Data Assimilation (SODA) are decomposed into four terms. The first term is the zonally averaged monthly climatological SST ([Tt(ϕ)]), which features relatively warm surface waters in the tropical IO and relatively colder surface waters over the southern IO. This term also has a relatively low SST pool between the Equator and 20°N. The SST at the center of the pool in summer is about 1-2°C lower than in spring and autumn. The second term is the spatially-varying monthly climatological SSTA (Tt*(λ,ϕ)), due mainly to the topographic effect and seasonal variation in wind forcing. The values of Tt*(λ,ϕ) are negative over the western coastal waters and positive over the eastern coastal and shelf waters in the tropical and northern IO. The third term is the zonally-averaged transient SSTA([T(ϕ,t)']Y). The largest values of [T(ϕ,t)']Y occur over the subtropical and mid-latitudes of the IO, which differs from the SSTA in the tropical waters of the Pacific Ocean. Time series of zonally and meridionally averaged T(ϕ,t)'Y in the tropical-subtropical IO is strongly correlated with the Indian Ocean basin-wide (IOBW) mode. The fourth term is the spatially-varying transient SSTA (T(λ,ϕ,t)*Y']. The REOF analysis of the fourth term demonstrates that the first REOF is correlated strongly with the South Indian Ocean Dipole (SIOD) mode. The second REOF is correlated strongly with the equatorial Indian Ocean dipole (IOD) mode. The third REOF is highly correlated with the tropical IOBW mode.

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Articles

Bartolomeo Doronzo, Stefano Taddei, Carlo Brandini
135 Views, 100 PDF Downloads
In a previous study an improved Maximum Cross-Correlation technique, called Multi-Window Maximum Cross-Correlation (MW-MCC), was proposed, and applied to noise-free synthetic images in order to show its potential and limits in oceanographic applications. In this work, instead, the application of MW-MCC to high resolution MODIS images, and its capability to provide useful and realistic results for ocean currents, is studied. When applied to real satellite images, the MW-MCC is subject to cloud cover and image quality problems. As a consequence the number of useful MODIS images is greatly reduced. However, for every MODIS image, multiple spec-tral bands are available, and it is possible to apply the MW-MCC algorithm to the same scene as many times as the number of these bands, increasing the possibility of finding valid current vectors. Moreover, the comparison among the results from different spectral bands allows to verify both the consistency of the computed current vectors and the validity of using a spectral band as a good tracer for the ocean circulation. Due to the lack of systematic current measurements in the area considered, it has been not possible to perform an ex-tensive error analysis of the MW-MCC results, although a case study of a comparison between HF radar measurements and MW-MCC data is shown. Moreover, some comparison between numerical ocean model simulations and MW-MCC results are also shown. The coherence of the resulting circulation flow, the high number of current vectors found, the agreement among different spectral bands, and conformity with the currents measured by the HF radars or simulated by hydrodynamic models show the validity of the technique.
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Articles

Yuhong Zhang, Junyao Chen, Yan Du
146 Views, 109 PDF Downloads
With the remarkable intensity of 170 knots, Typhoon Haiyan starts as a tropical depression on November 3 and develops to the peak as super tropical cyclone (TC) on November 7 in 2013. This intensity makes Haiyan one of the strongest TCs record ever observed and 35 knots higher than the maximum of the existing highest category. Haiyan originated from the eastern part of the Northwest Pacific Warm Pool and moved westward over warm water with a thick barrier layer (BL). The BL reduced the vertical mixing and entrainment caused by Haiyan and prevented the cold thermocline water into the mixed layer (ML). As a result, sea temperature cooling associated with wind stirring was suppressed. Relative high sea surface temperature (SST) kept fueling Haiyan via latent heat flux release, which favored the rapid development of a "Category 6" super typhoon.
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Articles

Douglas E Pirhalla, Scott C Sheridan, Cameron C Lee, Brian B Barnes, Varis Ransibrahmanakul, Chuanmin Hu
124 Views, 90 PDF Downloads
Temporal variability in water clarity for South Florida’s marine ecosystems was examined through satellite-derived light attenuation (Kd) coefficients, in the context of wind- and weather patterns. Reduced water clarity along Florida’s coasts is often the result of abrupt wind-resuspension events and other exogenous factors linked to frontal passage, storms, and precipitation. Kd data between 1998 and 2013 were synthesized to form a normalized Kd index (KDI) and subsequently compared with Self Organizing Map (SOM)-based wind field categorizations to reveal spatiotemporal patterns and their inter-relationships. Kd climatological maximums occur from October through December along southern sections of the West Florida Shelf (WFS) and from January through March along the Florida Straits. Spatial clusters of elevated Kd occur along 3 spatial domains: central WFS, southern WFS, and Florida Straits near the Florida Reef Tract, where intra-seasonal variability is the highest, and clarity patterns are associated with transitional wind patterns sequenced with cyclonic circulation. Temporal wind transitions from southerly to northerly, typically accompanying frontal passages, most often result in elevated Kd response. Results demonstrate the potential of using synoptic climatological analysis and satellite indices for tracking variability in water clarity and other indicators related to biological health.
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Indexing and Archiving

Archiving and Indexing Road Map

Satellite Oceanography and Meteorology (SOM) aims to be indexed by world-recognized databases, for example, PubMed, Scopus and Science Citation Index (SCI). SOM has been indexed and archived by several databases:

          

Editorial Board

Click here to see the editorial board.

Focus and Scope

The Satellite Oceanography and Meteorology (SOM) was launched in 2016, in response to the growing use of remotely sensed satellite data in understanding and identifying important processes and phenomena occurring in the atmosphere and ocean. The SOM provides space for oceanographers, meteorologists, hydrologists and climatologists to publish their research papers on theory, science, technology and applications of satellite remote sensing data of the ocean, atmosphere and climate.

For Authors

  • A manuscript would not be accepted if it has been published or is currently under consideration for publication in any other journals. The author will need to notify the editorial team if the data in their submission has been presented in conferences.

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    For more information on submission’s format, please refer to the ‘Author Guidelines’ link accessible from the ‘About’ button at the top row of this page.

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    Before your submission, please check that your manuscript has been prepared in accordance to the step-by-step instructions for submitting a manuscript to our online submission system.

    Manuscript Format

    Your manuscript should be in MS Word or LaTeX format. You are advised to download the document, Instructions for typesetting manuscripts (which can be found on http://som.whioce.com), as a template or for more details on preparing your submissions to Journal of Satellite Oceanography and Meteorology for consideration.

    All manuscripts must be written in clear, comprehensible English. Both British and American English are accepted. Usage of non-English words should be kept to a minimum and all must be italicized with the exception of “e.g.”, “i.e.” and “etc.” If you have concerns about the level of English in your submission, please ensure that it is proofread before submission by a native English speaker or a scientific editing service.

    Types of Submissions Accepted

    Satellite Oceanography and Meteorology accepts original articles, reviews, letters, editorials, commentaries, perspectives and position papers. Please read further for the definition of each type and select the appropriate option in the submission system. Submissions exceeding the suggested requirements such as ‘entire manuscript length’ will still be processed for consideration and peer review. However, article processing charges will differ in exceptional cases (e.g. the raw text file exceeds 2MB etc.) The article processing charge will then be determined on a case-by-case basis.

    Original articles: scientific articles on original basic and applied research and/or analysis. This manuscript type typically has 15 tables and figures in total, and approximately 100 references and 7,000 words (inclusive of reference list and abstract)

    Review articles: a summary highlighting recent developments and current/future trends of the field. This manuscript type typically has 10 tables and figures in total, and approximately 70 references and 7,000 words (inclusive of reference list and abstract)

    Letters to the Editor-in-Chief/authorship (please specify): comments from reader(s) about individual articles. These letters must be constructive and contribute to the development of individual articles published or the entire journal. Letters containing new ideas, supporting data or data criticizing the article may be subjected to peer-review (determined on a case-by-case basis by the journal’s editorial team) and published in the online publication but not in the printed version. This manuscript type typically has 1,800 words (exclusive of reference list)

    Editorials: Solicited concise commentary highlighting prominent topics in the Journal issue. These are the official opinions of the editors of the journal or special issue. Editorials will be published in both online and printed versions of the journal. This manuscript type typically has 3,500 words.

    Commentaries: Unsolicited commentaries or analysis from reader(s) targeting specific published articles in the journal. Commentaries will be subjected to peer-review and may be published in both online and printed versions of the journal. This manuscript type typically has 3,500 words.

    Perspectives articles: These are author’s personal opinions on a subject/topic. Unlike Review articles, Perspective articles may cover a more specific, narrow part of the field. However, these are still required to uphold the spirit of academia to be objective as well as aim to initiate or further discussions and novel experimental procedures in the field. Therefore, it will undergo peer review and be indexed if accepted. Accepted articles may be solicited or unsolicited. This manuscript type typically has 5 tables and figures in total and approximately 70 references and 7,000 words (inclusive of reference list and abstract).

    Position papers: Submissions that reflect the official opinion of an organization (e.g. government bodies, funding agencies etc.) This manuscript type typically has 3,500 words.

    Cover Letter

    All submissions should include a cover letter as a separate file. A cover letter should contain a brief explanation of what was previously known, the conceptual advancement with the findings and its significance to broad readership. The cover letter is confidential and will be read only by the editors. It will not be seen by reviewers.

    Title

    The title should capture the conceptual significance for a broad audience. The title should not be more than 50 words and should be able to give readers an overall view of the paper’s significance. Titles should avoid using uncommon jargons, abbreviations and punctuation.

    List of Authors

    The names of authors must be spelled out rather than set in initials along with their affiliations. Authors should be listed according to the extent of their contribution, with the major contributor listed first. All corresponding authors should be identified with an asterisk. Affiliations should contain the following core information: department, institution, city, state, postal code, and country. For contact, email address of at least one corresponding author must be included. Please note that all authors must see and approve the final version of the manuscript before submitting.

    Abstract

    Articles must include an abstract containing a maximum of 200 words. The purpose of abstract is to provide sufficient information for a reader to determine whether or not to proceed to the full text of the article. After the abstract, please give 5–8 key words; please avoid using the same words as those already used in the title.

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    Section Headings

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    Introduction

    Introduction should provide a background that gives a broad readership an overall outlook of the field and the research performed. It tackles a problem and states its importance regarding the significance of the study. Introduction can conclude with a brief statement of the aim of the work and a comment about whether that aim was achieved.

    Materials and Methods

    This section provides the general experimental design and methodologies used. The aim is to provide enough details for other investigators to fully replicate your results. It is also required to facilitate better understanding of the results obtained. Protocols and procedures for new methods must be included in detail to reproduce the experiments.

    Results

    This section can be divided into subheadings. This section focuses on the results of the experiments performed.

    Discussion

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    Conclusion

    Please use the conclusion section for interpretation only, and not to summarize information already presented in the text or abstract.

    Conflict of Interest

    All authors are required to declare all activities that have the potential to be deemed as a source of competing interest in relations to their submitted manuscript. Examples of such activities could include personal or work-related relationships, events, etc. Authors who have nothing to declare are encouraged to add "No conflict of interest was reported by all authors" in this section.

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    Authors should declare all financial and non-financial support that have the potential to be deemed as a source of competing interest in relations to their submitted manuscript in this section. Financial supports are generally in the form of grants, royalties, consulting fees and more. Examples of non-financial support could include the following: externally-supplied equipments/biological sources, writing assistance, administrative support, contributions from non-authors etc.

    Appendix

    This section is optional and is for all materials (e.g. advanced technical details) that has been excluded from the main text but remain essential to readers in understanding the manuscripts. This section is not for supplementary figures. Authors are advised to refer to the section on ‘Supplementary figures’ for such submissions.

    Figures

    Authors should include all figures into the manuscript and submit it as one file. Figures include photographs, scanned images, graphs, charts and schematic diagrams. Figures submitted should avoid unnecessary decorative effects (e.g. 3D graphs) as well as be minimally processed (e.g. changes in brightness and contrast applied uniformly for the entire figure). It should also be set against a white background. Please remember to label all figures (e.g. axis etc.) and number them (e.g. Figure 1, Figure 2, etc.) in boldface. Please also add in captions (below the figure) as required and number them (e.g. Figure 1, Figure 2, etc.) in bold-face. The caption should describe the entire figure without citing specific panels, followed by a legend defined as description of each panel. Please identify each panel with uppercase letters in parenthesis (e.g. (A), (B), (C), etc.)

    The preferred file formats for any separately submitted figure(s) are TIFF or JPEG. All figures should be legible in print form and of optimal resolution. Optimal resolutions preferred are 300 dots per inch for RBG colored, 600 dots per inch for greyscale and 1200 dots per inch for line art. Although there are no file size limitation imposed, authors are highly encouraged to compress their figures to an ideal size without unduly affecting legibility and resolution of figures. This will also speed up the process of uploading in the submission system if necessary.

    The Editor-in-Chief and Publisher reserve the right to request from author(s) the high-resolution files and unprocessed data and metadata files should the need arise at any point after manuscript submission for reasons such as production, evaluation or other purposes. The file name should allow for ease in identifying the associated manuscript submitted.

    Tables, Lists and Equations

    Tables created using Microsoft Word table function are preferred. The tables should include a title at the top. Titles and footnotes/legends should be concise. These must be submitted together with the manuscript. Likewise, lists and equations should be properly aligned and its meaning clear to readers. For listing things within the main body of the manuscript, please use roman numbers in parenthesis (e.g. (i), (ii), (iii), (iv), etc.)

    Supplementary Information

    This section is optional and contains all materials and figures that have been excluded from the entire manuscript. These materials are relevant to the manuscript but remain non-essential to readers’ understanding of the manuscript’s main content. All supplementary information should be submitted as a separate file in Step 4 during submission. Please ensure the names of such files contain ‘suppl. info’. Videos may be included in this section.

    In-text Citations

    Reference citations in the text should be done using the author-date method in which the author’s surname and the year published are included in the text. If the reference has no known year of publication, use ‘n.d.’ (without the quotation marks). The citation style depends on the number of authors for the reference.

    Examples:

    One author 

    Niemi (2011) illustrated some scenarios to prove this. The theory governs civil society (Niemi, 2011) and social behaviour. In 2011 Niemi described the theory in detail.

    Two authors

    Always use both names. Examples:

    Chandler and Tsai (2001) analyzed data from several reports. This theory was further supported by Chandler and Tsai (2001). In 2001 Chandra and Tsai proposed a possible mitigation measure.

    Three or more authors

    Use first author’s name, followed by italicized et al. and the year. Examples:

    Dickson et al. (2014) brought up some points to support such an argument. This was further emphasized (Dickson et al, 2014) and subsequently widely accepted. In 2014 Dickson et al. noted that such initiatives have far-bearing effects.

    Personal communications and unpublished works can only be used in the main text of the submission and are not to be placed in the Reference section. Authors are advised to limit such usage to the minimum. They should also be easily identifiable by stating the authors and year of such unpublished works or personal communications and the word ‘Unpublished’ in parenthesis.

    E.g. (Smith J, 2000, Unpublished)

    References

    This section is compulsory and should be placed at the end of all manuscripts. Do not use footnotes or endnotes as a substitute for a reference list. The list of references should only include works that are cited in the text and that have been published or accepted for publication. Personal communications and unpublished works should be excluded from this section.

    The references in reference list are arranged in alphabetical order of the first author’s surname. Authors referenced are listed with their surname followed by their initials. All references should also appear as an in-text citation. References should follow the following pattern: Author(s) followed by year of publication, title of publication, abbreviated journal name in italics, volume number, issue number in parenthesis and lastly, page range. If the referred article has more than three authors, list only the first three authors and abbreviate the remaining authors to italicized ‘et al.’ (meaning: "and others"). If the DOI is available, please include it after the page range.

    Journal article (print) with one to three  authors

    Younger P. (2004). Using the internet to conduct a literature search. Nurs Stand, 19(6): 45–51.

    Journal article (print) with more than three authors

    Gamelin F X, Baquet G, Berthoin S, et al. (2009). Effect of high intensity intermittent training on heart rate variability in prepubescent children. Eur J Appl Physiol, 105(1): 731–738.

    Journal article (online) with one to three authors

    Jackson D, Firtko A and Edenborough M. (2007). Personal resilience as a strategy for surviving and thriving in the face of workplace adversity: A literature review. J Adv Nurs, 60(1):  1–9. http://dx.doi.org/10.1111/j.1365-2648.2007.04412.x.

    Journal article (online) with more than three authors

    Hargreave M, Jensen A, Nielsen T S S, et al. (2015). Maternal use of fertility drugs and risk of cancer in children—A nationwide population-based cohort  study in Denmark. Int J Cancer, 136(8): 1931–1939. http://dx.doi.org/10.1002/ijc.29235.

    Book with one to three authors

    Schneider Z, Whitehead D and Elliott D. (2007). Nursing and Midwifery Research: Methods and Appraisal for Evidence-based Practice, 3rd edn. Marrickville, NSW: Elsevier Australia.

    Book with more than three authors

    Davis M, Charles L, Curry M J, et al. (2003). Challenging Spatial Norms, London: Routledge.

  • The names and email addresses entered in this journal site will be used exclusively for the stated purposes of this journal and will not be made available for any other purpose or to any other party.

Article Processing Charges (APC)

Satellite Oceanography and Meteorology is an Open Access Journal under Whioce Publishing. All articles published in Satellite Oceanography and Meteorology are accessible electronically from the journal website without commencing any kind of payment. In order to ensure contents are freely available and maintain publishing quality, Article Process Charges (APC) is applicable to all authors who wish to submit their articles to the journal to cover the cost incurred in processing the manuscripts. Such cost will cover the peer-review, copyediting, typesetting, publishing, content depositing and archiving processes. Those charges are applicable only to authors who have their manuscript successfully accepted after peer-review.

Journal TitleAPC
Satellite Oceanography and Meteorology$800

We encourage authors to publish their papers with us and don’t wish the cost of article processing fees to be a barrier especially to authors from the low and lower middle income countries/regions. A range of discounts or waivers are offered to authors who are unable to pay our publication processing fees. Authors can write in to apply for a waiver and requests will be considered on a case-by-case basis.

Authors based in these countries/regions listed below may apply to receive up to a 50%-100% waiver of the standard article processing fee; Waiver subjected to approval.

  • Afghanistan
  • Armenia
  • Bangladesh
  • Benin
  • Bhutan
  • Bolivia
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If you are residing in one of the above mentioned countries and need to apply for a waiver, please email our editorial department (editorial@whioce.com) with the following information:

  • Your name and institution with full address details
  • Title of journal you wish to submit a manuscript to
  • Reason for applying for a waiver
  • Title of your paper
  • Country of residence of all co-author

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Frequently Asked Questions

  • Answer: To establish whether your paper is suitable for this journal, please read Focus and Scope under Editorial Policies.
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Announcements

 

Call for Papers

 

The Editor-in-Chief, Prof. Jinyu Sheng, invites all authors to submit manuscripts for peer-review.

 
Posted: 2017-08-23
 
More Announcements...