Example of Boundary-Layer Meteorology format
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Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format
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Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format Example of Boundary-Layer Meteorology format
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open access Open Access

Boundary-Layer Meteorology — Template for authors

Publisher: Springer
Categories Rank Trend in last 3 yrs
Atmospheric Science #30 of 124 -
journal-quality-icon Journal quality:
High
calendar-icon Last 4 years overview: 349 Published Papers | 2092 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 24/06/2020
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Related Journals

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IEEE

Quality:  
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SJR: 1.246
SNIP: 1.579
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CiteRatio: 13.5
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American Meteorological Society

Quality:  
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CiteRatio: 4.1
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American Meteorological Society

Quality:  
High
CiteRatio: 9.8
SJR: 3.315
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Journal Performance & Insights

Impact Factor

CiteRatio

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.

A measure of average citations received per peer-reviewed paper published in the journal.

3.011

4% from 2018

Impact factor for Boundary-Layer Meteorology from 2016 - 2019
Year Value
2019 3.011
2018 3.149
2017 2.607
2016 2.573
graph view Graph view
table view Table view

6.0

9% from 2019

CiteRatio for Boundary-Layer Meteorology from 2016 - 2020
Year Value
2020 6.0
2019 5.5
2018 4.8
2017 4.5
2016 4.6
graph view Graph view
table view Table view

insights Insights

  • Impact factor of this journal has decreased by 4% in last year.
  • This journal’s impact factor is in the top 10 percentile category.

insights Insights

  • CiteRatio of this journal has increased by 9% in last years.
  • This journal’s CiteRatio is in the top 10 percentile category.

SCImago Journal Rank (SJR)

Source Normalized Impact per Paper (SNIP)

Measures weighted citations received by the journal. Citation weighting depends on the categories and prestige of the citing journal.

Measures actual citations received relative to citations expected for the journal's category.

1.107

14% from 2019

SJR for Boundary-Layer Meteorology from 2016 - 2020
Year Value
2020 1.107
2019 1.284
2018 1.348
2017 1.262
2016 1.525
graph view Graph view
table view Table view

1.472

8% from 2019

SNIP for Boundary-Layer Meteorology from 2016 - 2020
Year Value
2020 1.472
2019 1.366
2018 1.381
2017 1.211
2016 1.342
graph view Graph view
table view Table view

insights Insights

  • SJR of this journal has decreased by 14% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

  • SNIP of this journal has increased by 8% in last years.
  • This journal’s SNIP is in the top 10 percentile category.
Boundary-Layer Meteorology

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Springer

Boundary-Layer Meteorology

Boundary-Layer Meteorology publishes papers on the physical, chemical and biological processes occurring in the lowest few kilometres of the Earth's atmosphere. During its existence, Boundary-Layer Meteorology has become the primary medium for the publication of theoretical, n...... Read More

Atmospheric Science

Earth and Planetary Sciences

i
Last updated on
24 Jun 2020
i
ISSN
0006-8314
i
Impact Factor
High - 1.607
i
Open Access
No
i
Sherpa RoMEO Archiving Policy
Green faq
i
Plagiarism Check
Available via Turnitin
i
Endnote Style
Download Available
i
Bibliography Name
SPBASIC
i
Citation Type
Author Year
(Blonder et al, 1982)
i
Bibliography Example
Blonder GE, Tinkham M, Klapwijk TM (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

Journal Article DOI: 10.1007/BF00117978
A parametric model of vertical eddy fluxes in the atmosphere
Jean-François Louis1

Abstract:

A scheme for the representation of the vertical eddy fluxes of heat, momentum and water vapour in a forecast model is presented. An important feature of the scheme is the dependence of the diffusion coefficients on the static stability of the atmosphere. Two tests are presented, using the scheme in a one-dimensional model: th... A scheme for the representation of the vertical eddy fluxes of heat, momentum and water vapour in a forecast model is presented. An important feature of the scheme is the dependence of the diffusion coefficients on the static stability of the atmosphere. Two tests are presented, using the scheme in a one-dimensional model: the simulation of the diurnal cycle, and the transformation of a polar air mass moving over the warm sea. read more read less

Topics:

Diurnal cycle (53%)53% related to the paper, Atmosphere (52%)52% related to the paper
2,357 Citations
Journal Article DOI: 10.1023/A:1018966204465
Sonic anemometer tilt correction algorithms
James M. Wilczak1, Steven P. Oncley2, Steven A. Stage

Abstract:

The sensitivity of sonic anemometer-derived stress estimates to the tilt of the anemometer is investigated. The largest stress errors are shown to occur for unstable stratification (z/L<0) and deep convective boundary layers. Three methods for determining the tilt angles relative to a mean streamline coordinate system and for... The sensitivity of sonic anemometer-derived stress estimates to the tilt of the anemometer is investigated. The largest stress errors are shown to occur for unstable stratification (z/L<0) and deep convective boundary layers. Three methods for determining the tilt angles relative to a mean streamline coordinate system and for computing the tilt-corrected stresses are then compared. The most commonly used method, involving a double rotation of the anemometers' axes, is shown to result in significant run-to-run stress errors due to the sampling uncertainty of the mean vertical velocity. An alternative method, requiring a triple rotation of the anemometer axes, is shown to result in even greater run-to-run stress errors due to the combined sampling errors of the mean vertical velocity and the cross-wind stress. For measurements over the sea where the cross-stream stress is important, the double rotation method is shown to overestimate the surface stress, due to the uncorrected lateral tilt component. A third method, using a planar fit technique, isshown to reduce the run-to-run stress errors due to sampling effects, and provides an unbiased estimate of the lateral stress. read more read less

Topics:

Anemometer (51%)51% related to the paper
1,642 Citations
Journal Article DOI: 10.1007/BF00119502
Stratocumulus-capped mixed layers derived from a three-dimensional model
James W. Deardorff1

Abstract:

Results of a three-dimensional numerical model are analysed in a study of turbulence and entrainment within mixed layers containing stratocumulus with or without parameterized cloud-top radiative cooling. The model eliminates most of the assumptions invoked in theories of cloud-capped mixed layers, but suffers disadvantages w... Results of a three-dimensional numerical model are analysed in a study of turbulence and entrainment within mixed layers containing stratocumulus with or without parameterized cloud-top radiative cooling. The model eliminates most of the assumptions invoked in theories of cloud-capped mixed layers, but suffers disadvantages which include poor resolution and large truncation errors in and above the capping inversion. For relatively thick mixed layers with relatively thick capping inversions, the cloud-top radiative cooling is found to be lodged mostly within the capping inversion when the cooling is confined locally to the upper 50 m or less of the cloud. It does not then contribute substantially towards increased buoyancy flux and turbulence within the well mixed layer just below. The optimal means of correlating the entrainment rate, or mixed-layer growth rate, for mixed layers of variable amounts of stratocumulus is found to be through functional dependence upon an overall jump Richardson number, utilizing as scaling velocity the standard deviation of vertical velocity existing at the top of the mixed layer (near the center of the capping inversion). This velocity is found to be a fraction of the generalized convective velocity for the mixed layer as a whole which is greater for cloud-capped mixed layers than for clear mixed layers. read more read less

Topics:

Mixed layer (62%)62% related to the paper, Capping inversion (61%)61% related to the paper, Richardson number (51%)51% related to the paper
1,614 Citations
Journal Article DOI: 10.1007/BF00240838
A review of flux-profile relationships
A. J. Dyer1

Abstract:

Flux-profile relationships in the constant flux layer are reviewed The preferred relationships are found to be those of Dyer and Hicks (1970), namely, φ H =φ W =(1−16(z/L))−1/2, φ M =(1−16(z/L))−1/4 for the unstable region, and φ H =φ W =φ M = 1+5(z/L) for the stable region The carefully determined results o... Flux-profile relationships in the constant flux layer are reviewed The preferred relationships are found to be those of Dyer and Hicks (1970), namely, φ H =φ W =(1−16(z/L))−1/2, φ M =(1−16(z/L))−1/4 for the unstable region, and φ H =φ W =φ M = 1+5(z/L) for the stable region The carefully determined results of Businger et al (1971) remain a difficulty which calls for considerable clarification read more read less

Topics:

Flux (50%)50% related to the paper
1,564 Citations
Journal Article DOI: 10.1007/BF00122754
Frequency response corrections for eddy correlation systems

Abstract:

Simplified expressions describing the frequency response of eddy correlation systems due to sensor response, path-length averaging, sensor separation and signal processing are presented. A routine procedure for estimating and correcting for the frequency response loss in flux and variance measurements is discussed and illustr... Simplified expressions describing the frequency response of eddy correlation systems due to sensor response, path-length averaging, sensor separation and signal processing are presented. A routine procedure for estimating and correcting for the frequency response loss in flux and variance measurements is discussed and illustrated by application to the Institute of Hydrology's ‘Hydra’ eddy correlation system. The results show that flux loss from such a system is typically 5 to 10% for sensible and latent heat flux, but can be much larger for momentum flux and variance measurements in certain conditions. A microcomputer program is included which, with little modification, can be used for estimating flux loss from other eddy correlation systems with different or additional sensors. read more read less

Topics:

Frequency response (54%)54% related to the paper, Flux (52%)52% related to the paper, Latent heat (51%)51% related to the paper
1,204 Citations
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Boundary-Layer Meteorology format uses SPBASIC citation style.

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Frequently asked questions

1. Can I write Boundary-Layer Meteorology in LaTeX?

Absolutely not! Our tool has been designed to help you focus on writing. You can write your entire paper as per the Boundary-Layer Meteorology guidelines and auto format it.

2. Do you follow the Boundary-Layer Meteorology guidelines?

Yes, the template is compliant with the Boundary-Layer Meteorology guidelines. Our experts at SciSpace ensure that. If there are any changes to the journal's guidelines, we'll change our algorithm accordingly.

3. Can I cite my article in multiple styles in Boundary-Layer Meteorology?

Of course! We support all the top citation styles, such as APA style, MLA style, Vancouver style, Harvard style, and Chicago style. For example, when you write your paper and hit autoformat, our system will automatically update your article as per the Boundary-Layer Meteorology citation style.

4. Can I use the Boundary-Layer Meteorology templates for free?

Sign up for our free trial, and you'll be able to use all our features for seven days. You'll see how helpful they are and how inexpensive they are compared to other options, Especially for Boundary-Layer Meteorology.

5. Can I use a manuscript in Boundary-Layer Meteorology that I have written in MS Word?

Yes. You can choose the right template, copy-paste the contents from the word document, and click on auto-format. Once you're done, you'll have a publish-ready paper Boundary-Layer Meteorology that you can download at the end.

6. How long does it usually take you to format my papers in Boundary-Layer Meteorology?

It only takes a matter of seconds to edit your manuscript. Besides that, our intuitive editor saves you from writing and formatting it in Boundary-Layer Meteorology.

7. Where can I find the template for the Boundary-Layer Meteorology?

It is possible to find the Word template for any journal on Google. However, why use a template when you can write your entire manuscript on SciSpace , auto format it as per Boundary-Layer Meteorology's guidelines and download the same in Word, PDF and LaTeX formats? Give us a try!.

8. Can I reformat my paper to fit the Boundary-Layer Meteorology's guidelines?

Of course! You can do this using our intuitive editor. It's very easy. If you need help, our support team is always ready to assist you.

9. Boundary-Layer Meteorology an online tool or is there a desktop version?

SciSpace's Boundary-Layer Meteorology is currently available as an online tool. We're developing a desktop version, too. You can request (or upvote) any features that you think would be helpful for you and other researchers in the "feature request" section of your account once you've signed up with us.

10. I cannot find my template in your gallery. Can you create it for me like Boundary-Layer Meteorology?

Sure. You can request any template and we'll have it setup within a few days. You can find the request box in Journal Gallery on the right side bar under the heading, "Couldn't find the format you were looking for like Boundary-Layer Meteorology?”

11. What is the output that I would get after using Boundary-Layer Meteorology?

After writing your paper autoformatting in Boundary-Layer Meteorology, you can download it in multiple formats, viz., PDF, Docx, and LaTeX.

12. Is Boundary-Layer Meteorology's impact factor high enough that I should try publishing my article there?

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 these factors include review board, rejection rates, frequency of inclusion in indexes, and Eigenfactor. You need to assess all these factors before you make your final call.

13. What is Sherpa RoMEO Archiving Policy for Boundary-Layer Meteorology?

SHERPA/RoMEO Database

We extracted this data from Sherpa Romeo to help researchers understand the access level of this journal in accordance with the Sherpa Romeo Archiving Policy for Boundary-Layer Meteorology. The table below indicates the level of access a journal has as per Sherpa Romeo's 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.

14. What are the most common citation types In Boundary-Layer Meteorology?

The 5 most common citation types in order of usage for Boundary-Layer Meteorology are:.

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

15. How do I submit my article to the Boundary-Layer Meteorology?

It is possible to find the Word template for any journal on Google. However, why use a template when you can write your entire manuscript on SciSpace , auto format it as per Boundary-Layer Meteorology's guidelines and download the same in Word, PDF and LaTeX formats? Give us a try!.

16. Can I download Boundary-Layer Meteorology in Endnote format?

Yes, SciSpace provides this functionality. After signing up, you would need to import your existing references from Word or Bib file to SciSpace. Then SciSpace would allow you to download your references in Boundary-Layer Meteorology Endnote style according to Elsevier guidelines.

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I spent hours with MS word for reformatting. It was frustrating - plain and simple. With SciSpace, I can draft my manuscripts and once it is finished I can just submit. In case, I have to submit to another journal it is really just a button click instead of an afternoon of reformatting.

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