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Journal of Meteorological Research雜志CSCD期刊統(tǒng)計(jì)源期刊SCI期刊

  • 主管單位:中國(guó)科協(xié)

  • 主辦單位:中國(guó)氣象學(xué)會(huì)

  • ISSN:2095-6037

  • CN:11-2277/P

Journal of Meteorological Research雜志
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Journal of Meteorological Research雜志簡(jiǎn)介

CSCD期刊 統(tǒng)計(jì)源期刊 SCI期刊 科學(xué)類

《Journal of Meteorological Research》創(chuàng)刊于1987年,是中國(guó)氣象學(xué)會(huì)主辦、中國(guó)科協(xié)主管的全國(guó)性大氣科學(xué)學(xué)術(shù)性期刊.

《Journal of Meteorological Research》旨在對(duì)外反映我國(guó)大氣科學(xué)領(lǐng)域中最新科研成果,為大氣科學(xué)研究提供學(xué)術(shù)交流陣地,推動(dòng)我國(guó)大氣科學(xué)基礎(chǔ)研究和理論研究迅速發(fā)展,服務(wù)于我國(guó)氣象現(xiàn)代化建設(shè)事業(yè)。

《Journal of Meteorological Research》以氣象及水文、海洋、環(huán)境等相關(guān)學(xué)科的科研人員、高等院校師生為主要讀者對(duì)象,刊登動(dòng)力氣象學(xué)、天氣學(xué)、氣候?qū)W、數(shù)值天氣預(yù)報(bào)、大氣物理學(xué)、大氣化學(xué)、大氣探測(cè)、人工影響天氣及應(yīng)用氣象學(xué)等大氣科學(xué)各主要分支學(xué)科的代表我國(guó)研究新水平的創(chuàng)造性論文;國(guó)內(nèi)外大氣科學(xué)發(fā)展動(dòng)態(tài)的綜合評(píng)述;大氣科學(xué)新觀點(diǎn)、新理論、新技術(shù)、新方法的介紹;大氣科學(xué)研究工作簡(jiǎn)報(bào)及重要學(xué)術(shù)會(huì)議報(bào)道;國(guó)內(nèi)優(yōu)秀大氣科學(xué)專著的評(píng)介。

Journal of Meteorological Research雜志特色

重要注意事項(xiàng),請(qǐng)認(rèn)真閱讀

1.Manuscripts should be submitted with regular margins and the pages must be numbered consecutively . Brevity and lucidity are encouraged and papers each consisting of less than 25 pages include figures, tables, and references are preferred. Each manuscript generally includes the following components: (1) title, author's name, a±liation; (2) abstract; (3) key words; (4) text; (5) acknowledgment; (6) appendix; (7) references; and (8) tables and figures.

2.References should be arranged alphabetically without numbering at the end of the paper and the text citation should consist of the name of the author and the year of publication. The references for articles and books should be in the following form respectively:

1).Parasnis, S. S., and S. S. Goyal, 1989: Thermodynamic feature of the atmospheric boundary during the summer monsoon. Atmos. Environment, 24, 743- 753.

2).Zhang Jiabao, 1984: Intr oduction to Xinjiang Precipitation. China Meteorological Press, 14-16. (in Chinese)

3).Zeng Qingcun, 1994: Experiments of seasonal and extraseasonal predictions of summer monsoon precipitation. Proceedings of International Conference on Monsoon Variability and Predictability , Trieste, 9- 13 May 1994, 25-27.

3.Figures should be mentioned specifically and numbered consecutively in the text. All the figures are preferably made about twice final size and lettering should be large enough so that after reduction the smallest character will be at least 1.5 mm high. Give a detailed caption to each figure and note the approximate location of each figure and its caption in the text.

4.Tables should be typed directly at the appropriate locations in the text and arranged successively with Arabic numerals.

5.Footnotes, other than those which refer to the title heading, should be numbered successively and placed at the foot of the page to which they refer (not at the end of the paper). The authors requested to reduce the use of footnotes to a minimum.

6.The International System of Units should be used throughout. Words and symbols should not be mixed; in general, symbols should be used only when preceded by a number. Unit symbols are not punctuated, i.e., they are not treated as abbreviation; the same symbol is used for both singular and plural. Abbreviation should be avoided, especially of organizations, and acronyms should be identified with the first use. The other items not mentioned here should be dealt with according to the worldwide conventional rules.

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期刊數(shù)據(jù)庫(kù)收錄情況

期刊所獲榮譽(yù)

Journal of Meteorological Research統(tǒng)計(jì)數(shù)據(jù)

雜志各項(xiàng)綜合數(shù)據(jù)統(tǒng)計(jì)與評(píng)價(jià)

年度被引次數(shù)報(bào)告

2012 2013 2014 2015 2016 2017 2018 2019 2020 2021

本刊文章年份

2012 2011 2010 2009 2008 2007 2006 2005 2004 2003

在2012年的被引次數(shù)

10 22 21 28 11 13 7 17 5 11

被本刊自己引用的次數(shù)

1 5 1 5 1 2 0 0 1 1

被引次數(shù)的累積百分比

0.0439 0.1404 0.2325 0.3553 0.4035 0.4605 0.4912 0.5658 0.5877 0.636

本刊文章年份

2013 2012 2011 2010 2009 2008 2007 2006 2005 2004

在2013年的被引次數(shù)

3 37 30 27 20 8 10 8 16 6

被本刊自己引用的次數(shù)

1 1 8 6 0 0 0 1 0 0

被引次數(shù)的累積百分比

0.0121 0.1613 0.2823 0.3911 0.4718 0.504 0.5444 0.5766 0.6411 0.6653

本刊文章年份

2014 2013 2012 2011 2010 2009 2008 2007 2006 2005

在2014年的被引次數(shù)

7 26 35 29 29 31 12 14 14 6

被本刊自己引用的次數(shù)

3 13 5 5 5 5 1 1 7 1

被引次數(shù)的累積百分比

0.0247 0.1166 0.2403 0.3428 0.4452 0.5548 0.5972 0.6466 0.6961 0.7173

本刊文章年份

2015 2014 2013 2012 2011 2010 2009 2008 2007 2006

在2015年的被引次數(shù)

13 40 31 43 31 22 22 15 12 8

被本刊自己引用的次數(shù)

7 9 4 3 1 2 3 2 1 2

被引次數(shù)的累積百分比

0.04 0.1631 0.2585 0.3908 0.4862 0.5538 0.6215 0.6677 0.7046 0.7292

本刊文章年份

2016 2015 2014 2013 2012 2011 2010 2009 2008 2007

在2016年的被引次數(shù)

6 40 65 36 39 24 11 16 7 6

被本刊自己引用的次數(shù)

2 14 15 5 4 0 0 2 0 0

被引次數(shù)的累積百分比

0.0179 0.1373 0.3313 0.4388 0.5552 0.6269 0.6597 0.7075 0.7284 0.7463

本刊文章年份

2017 2016 2015 2014 2013 2012 2011 2010 2009 2008

在2017年的被引次數(shù)

14 37 43 52 36 42 20 12 18 11

被本刊自己引用的次數(shù)

7 12 12 12 2 2 3 2 1 2

被引次數(shù)的累積百分比

0.0394 0.1437 0.2648 0.4113 0.5127 0.631 0.6873 0.7211 0.7718 0.8028

本刊文章年份

2018 2017 2016 2015 2014 2013 2012 2011 2010 2009

在2018年的被引次數(shù)

11 46 52 38 55 23 22 15 22 8

被本刊自己引用的次數(shù)

3 17 13 7 7 2 1 1 2 0

被引次數(shù)的累積百分比

0.0297 0.1541 0.2946 0.3973 0.5459 0.6081 0.6676 0.7081 0.7676 0.7892

本刊文章年份

2019 2018 2017 2016 2015 2014 2013 2012 2011 2010

在2019年的被引次數(shù)

19 63 80 65 36 51 32 30 20 12

被本刊自己引用的次數(shù)

12 20 24 10 7 9 4 0 0 1

被引次數(shù)的累積百分比

0.0365 0.1577 0.3115 0.4365 0.5058 0.6038 0.6654 0.7231 0.7615 0.7846

本刊文章年份

2020 2019 2018 2017 2016 2015 2014 2013 2012 2011

在2020年的被引次數(shù)

24 53 66 76 42 31 54 26 23 18

被本刊自己引用的次數(shù)

14 26 20 15 9 4 12 4 1 3

被引次數(shù)的累積百分比

0.0449 0.1439 0.2673 0.4093 0.4879 0.5458 0.6467 0.6953 0.7383 0.772

本刊文章年份

2021 2020 2019 2018 2017 2016 2015 2014 2013 2012

在2021年的被引次數(shù)

10 56 46 57 71 48 56 28 33 9

被本刊自己引用的次數(shù)

4 18 13 9 12 6 3 0 3 0

被引次數(shù)的累積百分比

0.0205 0.1352 0.2295 0.3463 0.4918 0.5902 0.7049 0.7623 0.8299 0.8484
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