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Advances in Atmospheric Sciences — Template for authors

Publisher: Springer
Categories Rank Trend in last 3 yrs
Atmospheric Science #44 of 124 up up by 8 ranks
journal-quality-icon Journal quality:
Good
calendar-icon Last 4 years overview: 448 Published Papers | 2106 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 10/07/2020
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Related Journals

open access Open Access

IEEE

Quality:  
High
CiteRatio: 7.2
SJR: 1.246
SNIP: 1.579
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American Meteorological Society

Quality:  
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CiteRatio: 13.5
SJR: 3.367
SNIP: 2.93
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American Meteorological Society

Quality:  
High
CiteRatio: 4.1
SJR: 0.774
SNIP: 1.154
open access Open Access
recommended Recommended

American Meteorological Society

Quality:  
High
CiteRatio: 9.8
SJR: 3.315
SNIP: 1.909

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.

2.583

42% from 2018

Impact factor for Advances in Atmospheric Sciences from 2016 - 2019
Year Value
2019 2.583
2018 1.819
2017 1.869
2016 1.483
graph view Graph view
table view Table view

4.7

24% from 2019

CiteRatio for Advances in Atmospheric Sciences from 2016 - 2020
Year Value
2020 4.7
2019 3.8
2018 3.3
2017 2.9
2016 3.0
graph view Graph view
table view Table view

insights Insights

  • Impact factor of this journal has increased by 42% in last year.
  • This journal’s impact factor is in the top 10 percentile category.

insights Insights

  • CiteRatio of this journal has increased by 24% 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.

1.187

8% from 2019

SJR for Advances in Atmospheric Sciences from 2016 - 2020
Year Value
2020 1.187
2019 1.293
2018 1.14
2017 0.956
2016 0.974
graph view Graph view
table view Table view

1.186

9% from 2019

SNIP for Advances in Atmospheric Sciences from 2016 - 2020
Year Value
2020 1.186
2019 1.084
2018 0.938
2017 0.731
2016 0.784
graph view Graph view
table view Table view

insights Insights

  • SJR of this journal has decreased by 8% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

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

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Springer

Advances in Atmospheric Sciences

Approved by publishing and review experts on SciSpace, this template is built as per for Advances in Atmospheric Sciences formatting guidelines as mentioned in Springer author instructions. The current version was created on and has been used by 213 authors to write and format their manuscripts to this journal.

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Last updated on
09 Jul 2020
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ISSN
1861-9533
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Open Access
Hybrid
i
Sherpa RoMEO Archiving Policy
Green faq
i
Plagiarism Check
Available via Turnitin
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Endnote Style
Download Available
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Citation Type
Author Year
(Blonder et al, 1982)
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Bibliography Example
Beenakker CWJ (2006) Specular andreev reflection in graphene. Phys Rev Lett 97(6):067,007, URL 10.1103/PhysRevLett.97.067007

Top papers written in this journal

Journal Article DOI: 10.1007/BF02656915
The influence of ENSO on the summer climate change in China and its mechanism
Huang Ronghui1, Wu Yifang1

Abstract:

The influence of ENSO on the summer climate change in China and its mechanism from the observed data is discussed. It is discovered that in the developing stage of ENSO, the SST in the western tropical Pacific is colder in summer, the convective activities may be weak around the South China Sea and the Philippines. As a conse... The influence of ENSO on the summer climate change in China and its mechanism from the observed data is discussed. It is discovered that in the developing stage of ENSO, the SST in the western tropical Pacific is colder in summer, the convective activities may be weak around the South China Sea and the Philippines. As a consequence, the subtropical high shifted southward. Therefore, a drought may be caused in the Indo-China peninsula and in the South China. Moreover, in midsummer the subtropical high is weak over the Yangtze River valley and Huaihe River valley, and the flood may be caused in the area from the Yangtze River valley to Huaihe River valley. On the contrary, in the decaying stage of ENSO, the convective activities may be strong around the Philippines, and the subtropical high shifted northward, a drought may be caused in the Yangtze River valley and Huaihe River valley. read more read less

Topics:

Subtropical ridge (59%)59% related to the paper, Climate change in China (51%)51% related to the paper
567 Citations
Journal Article DOI: 10.1007/BF02919316
The weakening of the Asian monsoon circulation after the end of 1970's
Wang Huijun1

Abstract:

The transition of the global atmospheric circulation in the end of 1970's can clearly be detected in the atmospheric temperature, wind velocity, and so on. Wavelet analysis reveals that the temporal scale of this change is larger than 20 years. Studies in this work indicate that the trend of the transition over the mid-latitu... The transition of the global atmospheric circulation in the end of 1970's can clearly be detected in the atmospheric temperature, wind velocity, and so on. Wavelet analysis reveals that the temporal scale of this change is larger than 20 years. Studies in this work indicate that the trend of the transition over the mid-latitude Asia is opposite to that of global average for some variables at the middle troposphere. Another finding of this research is that the African-Asian monsoon circulation is weaker and the trade wind over the tropical eastern Pacific is weaker as well after this transition. Such a signal may be found in the summer precipitation over China as well. read more read less

Topics:

East Asian Monsoon (60%)60% related to the paper, Atmospheric circulation (56%)56% related to the paper, Wind speed (50%)50% related to the paper, Atmospheric temperature (50%)50% related to the paper
533 Citations
open accessOpen access Journal Article DOI: 10.1007/S00376-015-5192-6
Indo-Western Pacific Ocean Capacitor and Coherent Climate Anomalies in Post-ENSO Summer: A Review
Shang-Ping Xie1, Shang-Ping Xie2, Yu Kosaka3, Yan Du4, Kaiming Hu4, Jasti S. Chowdary5, Gang Huang4

Abstract:

ENSO induces coherent climate anomalies over the Indo-western Pacific, but these anomalies outlast SST anomalies of the equatorial Pacific by a season, with major effects on the Asian summer monsoon. This review provides historical accounts of major milestones and synthesizes recent advances in the endeavor to understand summ... ENSO induces coherent climate anomalies over the Indo-western Pacific, but these anomalies outlast SST anomalies of the equatorial Pacific by a season, with major effects on the Asian summer monsoon. This review provides historical accounts of major milestones and synthesizes recent advances in the endeavor to understand summer variability over the Indo-Northwest Pacific region. Specifically, a large-scale anomalous anticyclone (AAC) is a recurrent pattern in post-El Nino summers, spanning the tropical Northwest Pacific and North Indian oceans. Regarding the ocean memory that anchors the summer AAC, competing hypotheses emphasize either SST cooling in the easterly trade wind regime of the Northwest Pacific or SST warming in the westerly monsoon regime of the North Indian Ocean. Our synthesis reveals a coupled ocean-atmosphere mode that builds on both mechanisms in a two-stage evolution. In spring, when the northeast trades prevail, the AAC and Northwest Pacific cooling are coupled via wind-evaporation-SST feedback. The Northwest Pacific cooling persists to trigger a summer feedback that arises from the interaction of the AAC and North Indian Ocean warming, enabled by the westerly monsoon wind regime. This Indo-western Pacific ocean capacitor (IPOC) effect explains why El Nino stages its last act over the monsoonal Indo-Northwest Pacific and casts the Indian Ocean warming and AAC in leading roles. The IPOC displays interdecadal modulations by the ENSO variance cycle, significantly correlated with ENSO at the turn of the 20th century and after the 1970s, but not in between. Outstanding issues, including future climate projections, are also discussed. read more read less

Topics:

Pacific decadal oscillation (66%)66% related to the paper, North Pacific High (62%)62% related to the paper, East Asian Monsoon (61%)61% related to the paper, Ocean heat content (61%)61% related to the paper, Indian Ocean Dipole (60%)60% related to the paper
View PDF
482 Citations
Journal Article DOI: 10.1007/BF02973084
A diagnostic study of the impact of El Niño on the precipitation in China
Renhe Zhang1, Akimasa Sumi2, Masahide Kimoto2

Abstract:

The impact of El Nino on the precipitation in China for different seasons are investigated diagnostically. It is found that El Nino can influence the precipitation in China significantly during its mature phase. In the Northern winter, spring and autumn, the positive precipitation anomalies are found in the southern part of C... The impact of El Nino on the precipitation in China for different seasons are investigated diagnostically. It is found that El Nino can influence the precipitation in China significantly during its mature phase. In the Northern winter, spring and autumn, the positive precipitation anomalies are found in the southern part of China during the El Nino mature phase. In the Northern summer, the patterns of the precipitation anomalies in the El Nino mature phase are different from those in the other seasons. The negative precipitation anomalies appear in both southern and northern parts of China, while in between around the lower reaches of the Yangtze River and the Huaihe River valleys the precipitation anomalies tend to be positive. In the Northern winter, spring and autumn, the physical process by which El Nino affects the precipitation in the southern part of China can be explained by the features of the circulation anomalies over East Asia during the El Nino mature phase (Zhang et al., 1996). The appearance of an anticyclonic anomaly to the north of the maritime continent in the lower troposphere during the El Nino mature phase intensifies the subtropical high in the western Pacific and makes it shift westward. The associated southwesterly flow is responsible for the positive precipitation anomalies in the southern part of China. In the Northern summer, the intensified western Pacific subtropical high covers the southeastern periphery of China so that the precipitation there becomes less. In addition, the weakening of the Indian monsoon provides less moisture inflow to the northern part of China. read more read less

Topics:

Subtropical ridge (56%)56% related to the paper, East Asian Monsoon (54%)54% related to the paper, Monsoon of South Asia (53%)53% related to the paper, Anticyclone (51%)51% related to the paper, Precipitation (51%)51% related to the paper
435 Citations
Journal Article DOI: 10.1007/S00376-997-0016-Y
Climatology and Interannual Variability of the Southeast Asian Summer Monsoon
K. M. Lau1, Song Yang1

Abstract:

In this paper, results from a pilot study for the South China Sea Monsoon Experiment are reported. Based on analyses of 9 years of pentad and monthly mean data, the climatology of subseasonal features and interannual variability of the Southeast Asian monsoon (SEAM) are documented. The present analysis is focused on the sudde... In this paper, results from a pilot study for the South China Sea Monsoon Experiment are reported. Based on analyses of 9 years of pentad and monthly mean data, the climatology of subseasonal features and interannual variability of the Southeast Asian monsoon (SEAM) are documented. The present analysis is focused on the sudden onset of the South China Sea monsoon and its relation to the atmospheric and oceanic processes on the entire Asian monsoon region. It is found that the onset of the SEAM occurs around mid-May, signaling the earliest stage of the entire Asian summer monsoon system. The establishment of monsoon rainfall over the South China Sea is abrupt, being accompanied by substantial changes in the large scale atmospheric circulation and sea surface temperature in the adjacent oceans. The onset and fluctuations of SEAM involve the interaction and metamorphosis of the large scale convection over the Indo-China, the South China Sea and the southern Bay of Bengal. Results show that the onset time of the SEAM differs greatly from one year to another. The delayed (advanced) onset of the monsoon may be related to basin-wide warm (cold) events of the Pacific and Indian Oceans. We also present evidence showing that the SEAM fluctuations in May may foreshadow the development of the full-scale Asian summer monsoon during the subsequent months. read more read less

Topics:

East Asian Monsoon (71%)71% related to the paper, Monsoon (64%)64% related to the paper, Southeast asian (60%)60% related to the paper, Sea surface temperature (53%)53% related to the paper, Atmospheric circulation (51%)51% related to the paper
412 Citations
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Frequently asked questions

1. Can I write Advances in Atmospheric Sciences in LaTeX?

Absolutely not! Our tool has been designed to help you focus on writing. You can write your entire paper as per the Advances in Atmospheric Sciences guidelines and auto format it.

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Yes, the template is compliant with the Advances in Atmospheric Sciences 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 Advances in Atmospheric Sciences?

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 Advances in Atmospheric Sciences citation style.

4. Can I use the Advances in Atmospheric Sciences 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 Advances in Atmospheric Sciences.

5. Can I use a manuscript in Advances in Atmospheric Sciences 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 Advances in Atmospheric Sciences that you can download at the end.

6. How long does it usually take you to format my papers in Advances in Atmospheric Sciences?

It only takes a matter of seconds to edit your manuscript. Besides that, our intuitive editor saves you from writing and formatting it in Advances in Atmospheric Sciences.

7. Where can I find the template for the Advances in Atmospheric Sciences?

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 Advances in Atmospheric Sciences'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 Advances in Atmospheric Sciences'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.

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SciSpace's Advances in Atmospheric Sciences 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.

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11. What is the output that I would get after using Advances in Atmospheric Sciences?

After writing your paper autoformatting in Advances in Atmospheric Sciences, you can download it in multiple formats, viz., PDF, Docx, and LaTeX.

12. Is Advances in Atmospheric Sciences'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 Advances in Atmospheric Sciences?

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 Advances in Atmospheric Sciences. 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 Advances in Atmospheric Sciences?

The 5 most common citation types in order of usage for Advances in Atmospheric Sciences 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 Advances in Atmospheric Sciences?

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 Advances in Atmospheric Sciences's guidelines and download the same in Word, PDF and LaTeX formats? Give us a try!.

16. Can I download Advances in Atmospheric Sciences 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 Advances in Atmospheric Sciences Endnote style according to Elsevier guidelines.

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