Example of Asia-Pacific Journal of Atmospheric Sciences format
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Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format
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Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format Example of Asia-Pacific Journal of Atmospheric Sciences format
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Asia-Pacific Journal of Atmospheric Sciences — Template for authors

Publisher: Springer
Categories Rank Trend in last 3 yrs
Atmospheric Science #62 of 124 down down by 13 ranks
journal-quality-icon Journal quality:
Good
calendar-icon Last 4 years overview: 187 Published Papers | 636 Citations
indexed-in-icon Indexed in: Scopus
last-updated-icon Last updated: 19/07/2020
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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.

1.833

3% from 2018

Impact factor for Asia-Pacific Journal of Atmospheric Sciences from 2016 - 2019
Year Value
2019 1.833
2018 1.772
2017 1.344
2016 1.65
graph view Graph view
table view Table view

3.4

31% from 2019

CiteRatio for Asia-Pacific Journal of Atmospheric Sciences from 2016 - 2020
Year Value
2020 3.4
2019 2.6
2018 2.1
2017 3.0
2016 3.4
graph view Graph view
table view Table view

insights Insights

  • Impact factor of this journal has increased by 3% in last year.
  • This journal’s impact factor is in the top 10 percentile category.

insights Insights

  • CiteRatio of this journal has increased by 31% 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.

0.695

16% from 2019

SJR for Asia-Pacific Journal of Atmospheric Sciences from 2016 - 2020
Year Value
2020 0.695
2019 0.823
2018 0.743
2017 0.855
2016 1.057
graph view Graph view
table view Table view

0.936

6% from 2019

SNIP for Asia-Pacific Journal of Atmospheric Sciences from 2016 - 2020
Year Value
2020 0.936
2019 0.879
2018 0.748
2017 0.627
2016 0.92
graph view Graph view
table view Table view

insights Insights

  • SJR of this journal has decreased by 16% in last years.
  • This journal’s SJR is in the top 10 percentile category.

insights Insights

  • SNIP of this journal has increased by 6% in last years.
  • This journal’s SNIP is in the top 10 percentile category.

Asia-Pacific Journal of Atmospheric Sciences

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Springer

Asia-Pacific Journal of Atmospheric Sciences

The Asia-Pacific Journal of Atmospheric Sciences (APJAS) publishes original scientific research in all fields of atmospheric science, with emphasis on but not limited to theoretical/observational/numerical studies on meteorological, climatological, and atmospheric environmenta...... Read More

Atmospheric Science

Earth and Planetary Sciences

i
Last updated on
19 Jul 2020
i
ISSN
1976-7633
i
Impact Factor
Medium - 0.535
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
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

open accessOpen access Journal Article
The WRF Single-Moment 6-Class Microphysics Scheme (WSM6)

Abstract:

This study examines the performance of the Weather Research and Forecasting (WRF)-Single-Moment- Microphysics scheme (WSMMPs) with a revised ice-microphysics of the Hong et al. In addition to the simple (WRF Single-Moment 3-class Microphysics scheme; WSM3) and mixed-phase (WRF Single-Moment 5-class Microphysics scheme; WSM5) ... This study examines the performance of the Weather Research and Forecasting (WRF)-Single-Moment- Microphysics scheme (WSMMPs) with a revised ice-microphysics of the Hong et al. In addition to the simple (WRF Single-Moment 3-class Microphysics scheme; WSM3) and mixed-phase (WRF Single-Moment 5-class Microphysics scheme; WSM5) schemes of the Hong et al., a more complex scheme with the inclusion of graupel as another predictive variable (WRF Single-Moment 6-class Microphysics scheme; WSM6) was developed. The characteristics of the three categories of WSMMPs were examined for an idealized storm case and a heavy rainfall event over Korea. In an idealized thunderstorm simulation, the overall evolutionary features of the storm are not sensitive to the number of hydrometeors in the WSMMPs; however, the evolution of surface precipitation is significantly influenced by the complexity in microphysics. A simulation experiment for a heavy rainfall event indicated that the evolution of the simulated precipitation with the inclusion of graupel (WSM6) is similar to that from the simple (WSM3) and mixed-phase (WSM5) microphysics in a low-resolution grid; however, in a high-resolution grid, the amount of rainfall increases and the peak intensity becomes stronger as the number of hydrometeors increases. read more read less

Topics:

Microphysics (70%)70% related to the paper, Weather Research and Forecasting Model (54%)54% related to the paper, Graupel (52%)52% related to the paper
2,357 Citations
Journal Article DOI: 10.1007/S13143-013-0027-9
Synoptic analysis of dust storms in the Middle East
Mehdi Hamidi1, Mohammad Reza Kavianpour1, Yaping Shao2

Abstract:

Dust storm in the Middle East and south-west Asia is a natural hazard and the Tigris-Euphrates alluvial plain has been recognized as the main dust source in this area. In this study, more than 60 dust storms that occurred during the period 2003–2011 are investigated on the basis of MODIS satellite images, and 12 of the dust s... Dust storm in the Middle East and south-west Asia is a natural hazard and the Tigris-Euphrates alluvial plain has been recognized as the main dust source in this area. In this study, more than 60 dust storms that occurred during the period 2003–2011 are investigated on the basis of MODIS satellite images, and 12 of the dust storms are selected for synoptic analysis using the NCEP-NCAR Reanalysis Data. The potential dust sources in the Middle East and south-west Asian region (20°E to 80°E, 5°N to 50°N) are analyzed and used in the synoptic analysis. Dust storms in the region can be grouped into two main categories, i.e., the Shamal dust storms and the frontal dust storms. Synoptic systems, associated with the two categories, are distinguished and the frequency of the patterns is identified. For 68% of the Shamal dust storms, a high pressure system is situated between 0°E to 30°E and 27°N to 45°N, and a low pressure system between 50°E to 70°E and 23°N to 43°N. For 86% of the frontal dust storms, a high is located between 51°E to 67°E and 18°N to 33°N and a low between 28°E to 48°E and 32°N to 43°N. Three main patterns for Shamal dust storms are identified, which represent about 60% of the Shamal dust storms. This analysis confirms that the Shamal is related to the anticyclones located over northern Africa to Eastern Europe and the monsoon trough over Iraq, southern Iran, Pakistan and the Indian Subcontinent. The analysis also shows that the main dust sink for the frontal dust storms in Tigris and Euphrates alluvial plain extends from center of Iraq to west and center of Iran and, in most severe cases, to northern Iran and the southern coast of the Caspian Sea. read more read less

Topics:

Shamal (62%)62% related to the paper, Dust storm (59%)59% related to the paper, Storm (51%)51% related to the paper
View PDF
204 Citations
Journal Article DOI: 10.1007/S13143-013-0053-7
Climate change in the 21st century simulated by HadGEM2-AO under representative concentration pathways

Abstract:

We present climate responses of Representative Concentration Pathways (RCPs) using the coupled climate model HadGEM2-AO for the Coupled Model Intercomparison Project phase 5 (CMIP5). The RCPs are selected as standard scenarios for the IPCC Fifth Assessment Report and these scenarios include time paths for emissions and concen... We present climate responses of Representative Concentration Pathways (RCPs) using the coupled climate model HadGEM2-AO for the Coupled Model Intercomparison Project phase 5 (CMIP5). The RCPs are selected as standard scenarios for the IPCC Fifth Assessment Report and these scenarios include time paths for emissions and concentrations of greenhouse gas and aerosols and land-use/land cover. The global average warming and precipitation increases for the last 20 years of the 21st century relative to the period 1986-2005 are +1.1°C/+2.1% for RCP2.6, +2.4°C/+4.0% for RCP4.5, +2.5°C/+3.3% for RCP6.0 and +4.1°C/+4.6% for RCP8.5, respectively. The climate response on RCP 2.6 scenario meets the UN Copenhagen Accord to limit global warming within two degrees at the end of 21st century, the mitigation effect is about 3°C between RCP2.6 and RCP8.5. The projected precipitation changes over the 21st century are expected to increase in tropical regions and at high latitudes, and decrease in subtropical regions associated with projected poleward expansions of the Hadley cell. Total soil moisture change is projected to decrease in northern hemisphere high latitudes and increase in central Africa and Asia whereas near-surface soil moisture tends to decrease in most areas according to the warming and evaporation increase. The trend and magnitude of future climate extremes are also projected to increase in proportion to radiative forcing of RCPs. For RCP 8.5, at the end of the summer season the Arctic is projected to be free of sea ice. read more read less

Topics:

Global warming (60%)60% related to the paper, Representative Concentration Pathways (59%)59% related to the paper, Climate model (55%)55% related to the paper, Coupled model intercomparison project (54%)54% related to the paper, Climate change (54%)54% related to the paper
174 Citations
Journal Article DOI: 10.1007/S13143-014-0016-7
Urban impacts on precipitation
Ji-Young Han, Jong-Jin Baik1, Hyunho Lee1

Abstract:

Weather and climate changes caused by human activities (e.g., greenhouse gas emissions, deforestation, and urbanization) have received much attention because of their impacts on human lives as well as scientific interests. The detection, understanding, and future projection of weather and climate changes due to urbanization a... Weather and climate changes caused by human activities (e.g., greenhouse gas emissions, deforestation, and urbanization) have received much attention because of their impacts on human lives as well as scientific interests. The detection, understanding, and future projection of weather and climate changes due to urbanization are important subjects in the discipline of urban meteorology and climatology. This article reviews urban impacts on precipitation. Observational studies of changes in convective phenomena over and around cities are reviewed, with focus on precipitation enhancement downwind of cities. The proposed causative factors (urban heat island, large surface roughness, and higher aerosol concentration) and mechanisms of urban-induced and/or urban-modified precipitation are then reviewed and discussed, with focus on downwind precipitation enhancement. A universal mechanism of urban-induced precipitation is made through a thorough literature review and is as follows. The urban heat island produces updrafts on the leeward or downwind side of cities, and the urban heat island-induced updrafts initiate moist convection under favorable thermodynamic conditions, thus leading to surface precipitation. Surface precipitation is likely to further increase under higher aerosol concentrations if the air humidity is high and deep and strong convection occurs. It is not likely that larger urban surface roughness plays a major role in urbaninduced precipitation. Larger urban surface roughness can, however, disrupt or bifurcate precipitating convective systems formed outside cities while passing over the cities. Such urban-modified precipitating systems can either increase or decrease precipitation over and/or downwind of cities. Much effort is needed for in-depth or new understanding of urban precipitation anomalies, which includes local and regional modeling studies using advanced numerical models and analysis studies of long-term radar data. read more read less

Topics:

Urban climatology (61%)61% related to the paper, Urban heat island (55%)55% related to the paper, Precipitation (54%)54% related to the paper, Weather and climate (52%)52% related to the paper, Urbanization (52%)52% related to the paper
150 Citations
open accessOpen access Journal Article
Tropical Cyclone Structure (TCS08) Field Experiment Science Basis, Observational Platforms, and Strategy

Abstract:

The Tropical Cyclone Structure (TCS08) in cooperation with the THORPEX Pacific Asian Regional Campaign (T-PARC) during August and September 2008 is the most significant tropical cyclone-related field experiment in the western North Pacific since 1990. This article will summarize the science basis, observational platforms, and... The Tropical Cyclone Structure (TCS08) in cooperation with the THORPEX Pacific Asian Regional Campaign (T-PARC) during August and September 2008 is the most significant tropical cyclone-related field experiment in the western North Pacific since 1990. This article will summarize the science basis, observational platforms, and strategy for the TCS08. The tropical cyclone formation component of TCS08 will address the multi-scale aspects, but the primary focus will be on a ventilation hypothesis and a marsupial paradigm on the synoptic scale, and a top-down and a bottom-up hypothesis on the mesoscale. A number of numerical modeling, adjoint sensitivity and targeting, and observational studies are supporting the TCS08 formation component. The primary foci of the structure change component of TCS08 are changes associated with secondary eyewall formation, air-sea interaction impacts via boundary layer rolls and the ocean response and feedback, and understanding of superintensity. A major objective of the TCS08 structure change component is to make in situ observations of the intensity and structure and their changes for validating satellite-based techniques. Numerical modeling and data assimilation studies will also support the structure change component. The long-range lightning network in the western North Pacific is being augmented with at least five new stations and these observations will be correlated with intensity changes in conjunction with modeling studies. An open data policy applies to both TCS08 and T-PARC, and researchers are encouraged to collaborate in the field experiments and in the analyses, numerical modeling, and interpretations of the TCS08 data sets. read more read less

Topics:

Tropical cyclone (57%)57% related to the paper, Tropical cyclone scales (56%)56% related to the paper, Tropical cyclone forecast model (56%)56% related to the paper
145 Citations
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Asia-Pacific Journal of Atmospheric Sciences format uses SPBASIC citation style.

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Frequently asked questions

1. Can I write Asia-Pacific Journal of 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 Asia-Pacific Journal of Atmospheric Sciences guidelines and auto format it.

2. Do you follow the Asia-Pacific Journal of Atmospheric Sciences guidelines?

Yes, the template is compliant with the Asia-Pacific Journal of 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 Asia-Pacific Journal of 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 Asia-Pacific Journal of Atmospheric Sciences citation style.

4. Can I use the Asia-Pacific Journal of 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 Asia-Pacific Journal of Atmospheric Sciences.

5. Can I use a manuscript in Asia-Pacific Journal of 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 Asia-Pacific Journal of Atmospheric Sciences that you can download at the end.

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7. Where can I find the template for the Asia-Pacific Journal of Atmospheric Sciences?

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8. Can I reformat my paper to fit the Asia-Pacific Journal of 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.

9. Asia-Pacific Journal of Atmospheric Sciences an online tool or is there a desktop version?

SciSpace's Asia-Pacific Journal of 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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After writing your paper autoformatting in Asia-Pacific Journal of Atmospheric Sciences, you can download it in multiple formats, viz., PDF, Docx, and LaTeX.

12. Is Asia-Pacific Journal of 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 Asia-Pacific Journal of 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 Asia-Pacific Journal of 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 Asia-Pacific Journal of Atmospheric Sciences?

The 5 most common citation types in order of usage for Asia-Pacific Journal of 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 Asia-Pacific Journal of 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 Asia-Pacific Journal of Atmospheric Sciences's guidelines and download the same in Word, PDF and LaTeX formats? Give us a try!.

16. Can I download Asia-Pacific Journal of 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 Asia-Pacific Journal of Atmospheric Sciences Endnote style according to Elsevier guidelines.

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