投稿应注意的几个问题
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投稿应注意的几个问题
刘燕君
Editor of
Journal of Resources and Ecology 2010-12-15
内容
有创新 有重要应用意义 有充足的实验或分析 支持文章的结论
形式
规范 完整 语言简洁准确
形式——规范，完整
国家标准：
《科学技术期刊编排格式》》(GB/T3179-92) 《科学技术报告、学位论文和学术论文的编写格式》（GB 7714-87） 《文后参考文献著录规则》（GB/T7714-2005）
系统性 逻辑性 材料的安排前后有序 详略得当 标准 规范 美观 精度符合出版要求 设计合理 关系明确 顺序编码制 著者—出版年制
文题示例
A Determination of the Cloud Feedback from Climate Variations over the Past Decade El Niño Lends More Confidence to Strong Global Warming Ice-sheet Acceleration Driven by Melt Supply Variability Changes in Synoptic Weather Patterns and Greenland Precipitation in the 20th and 21st Centuries Analysis of 21st Century Atmospheric Changes Using Self-organizing Maps A Model for Turbulent Hydraulic Fracture and Application to Crack Propagation at Glacier beds
国家新闻出版总署：
《期刊出版形式规范》：
国内统一连续出版物号（CN） 、国际标准连续出版物号（ISSN）、 广告经营许可证号、期刊条码、期刊名称、期刊主要责任单位（主管 单位、主办单位、出版单位）、印刷发行单位、总编辑、期刊出版标 识（期刊编号、刊期）、版权页和期刊标识性文字
形式Biblioteka Baidu
文题 准确 简练
标题 图片 表格 参考文献
表格
Climate models disagree on the magnitude of the cloud feedback, simulating a range of cloud feedbacks in response to long-term global warming from near zero to a positive feedback of 1 W/m2/K (3, 4). This spread is the single most important reason for the large spread in the climate sensitivities among climate models (5, 6). Despite the importance of the cloud feedback, there have been few estimates of its magnitude from observations. Previous work has generally focused on just part of the problem [for example, the tropics (7, 8) or low clouds (9)], and these analyses differ even on the sign of the cloud feedback. ……
摘要 • Using “I” rather than “This paper” or passive voice • 注意从句的用法（定语从句，状语从句） • 体会介词的用法 • 没有过多的“the” (只有4个)
Estimates of Earth's climate sensitivity are uncertain, largely because of uncertainty in the long-term cloud feedback. I estimated the magnitude of the cloud feedback in response to short-term climate variations by analyzing the top-of-atmosphere radiation budget from March 2000 to February 2010. Over this period, the short-term cloud feedback had a magnitude of 0.54 ± 0.74 (2σ) watts per square meter per kelvin, meaning that it is likely positive. A small negative feedback is possible, but one large enough to cancel the climate’s positive feedbacks is not supported by these observations. Both long- and short-wave components of short-term cloud feedback are also likely positive. Calculations of short-term cloud feedback in climate models yield a similar feedback. I find no correlation in the models between the shortand long-term cloud feedbacks.
[1] Yang H, Li, X B. Cultivated land and food supply in China [J]. Land Use Policy, 2000, 17(2): 73-88. [2] Li Xiubin, Wang Xiuhong. Changes in agricultural land use in China: 1981 - 2000 [J]. Asian Geographer, 2003, 22(1-2):27-42. [3] MENG Ji-jun, FU Zai-yi. The research on the sustainable use of cultivated land resource in China. Areal Research and Development, 1998, 17(4):32-36. [4] LIU Cheng-wu, LI Xiu-bin. The changing characteristics of the agricultural land use intensity in China based on the production cost. Journal of Natural Resources, 2006, 21(1): 9-15. [5] ZHU Hui-yi, LI Xiu-bin, XIN Liang-jie. Intensity change in cultivated land use in China and its policy implications. Journal of Natural Resources, 2007, 22(6): 907-915. [6] LIU Cheng-wu, LI Xiu-bin. Regional differences in the changes of the agricultural land use in China during 1980-2002. Acta Geographica Sinica, 2006, 61(2): 139-145.
论文示例
http://www.nature.com/nature/journal/v468/n7325/full/nature09618.html#/references
http://www.sciencemag.org/content/330/6010/1523.full
Increased ice velocities in Greenland are contributing significantly to eustatic sea level rise. Faster ice flow has been associated with ice–ocean interactions in water-terminating outlet glaciers and with increased surface meltwater supply to the ice-sheet bed inland. Observed correlations between surface melt and ice acceleration have raised the possibility of a positive feedback in which surface melting and accelerated dynamic thinning reinforce one another, suggesting that overall warming could lead to accelerated mass loss. Here I show that it is not simply mean surface melt but an increase in water input variability that drives faster ice flow. Glacier sliding responds to melt indirectly through changes in basal water pressure, with observations showing that water under glaciers drains through channels at low pressure or through interconnected cavities at high pressure. Using a model that captures the dynamic switching between channel and cavity drainage modes, I show that channelization and glacier deceleration rather than acceleration occur above a critical rate of water flow. Higher rates of steady water supply can therefore suppress rather than enhance dynamic thinning, indicating that the melt/dynamic thinning feedback is not universally operational. Short-term increases in water input are, however, accommodated by the drainage system through temporary spikes in water pressure. It is these spikes that lead to ice acceleration, which is therefore driven by strong diurnal melt cycles and an increase in rain and surface lake drainage events rather than an increase in mean melt supply.
刘燕君
Editor of
Journal of Resources and Ecology 2010-12-15
内容
有创新 有重要应用意义 有充足的实验或分析 支持文章的结论
形式
规范 完整 语言简洁准确
形式——规范，完整
国家标准：
《科学技术期刊编排格式》》(GB/T3179-92) 《科学技术报告、学位论文和学术论文的编写格式》（GB 7714-87） 《文后参考文献著录规则》（GB/T7714-2005）
系统性 逻辑性 材料的安排前后有序 详略得当 标准 规范 美观 精度符合出版要求 设计合理 关系明确 顺序编码制 著者—出版年制
文题示例
A Determination of the Cloud Feedback from Climate Variations over the Past Decade El Niño Lends More Confidence to Strong Global Warming Ice-sheet Acceleration Driven by Melt Supply Variability Changes in Synoptic Weather Patterns and Greenland Precipitation in the 20th and 21st Centuries Analysis of 21st Century Atmospheric Changes Using Self-organizing Maps A Model for Turbulent Hydraulic Fracture and Application to Crack Propagation at Glacier beds
国家新闻出版总署：
《期刊出版形式规范》：
国内统一连续出版物号（CN） 、国际标准连续出版物号（ISSN）、 广告经营许可证号、期刊条码、期刊名称、期刊主要责任单位（主管 单位、主办单位、出版单位）、印刷发行单位、总编辑、期刊出版标 识（期刊编号、刊期）、版权页和期刊标识性文字
形式Biblioteka Baidu
文题 准确 简练
标题 图片 表格 参考文献
表格
Climate models disagree on the magnitude of the cloud feedback, simulating a range of cloud feedbacks in response to long-term global warming from near zero to a positive feedback of 1 W/m2/K (3, 4). This spread is the single most important reason for the large spread in the climate sensitivities among climate models (5, 6). Despite the importance of the cloud feedback, there have been few estimates of its magnitude from observations. Previous work has generally focused on just part of the problem [for example, the tropics (7, 8) or low clouds (9)], and these analyses differ even on the sign of the cloud feedback. ……
摘要 • Using “I” rather than “This paper” or passive voice • 注意从句的用法（定语从句，状语从句） • 体会介词的用法 • 没有过多的“the” (只有4个)
Estimates of Earth's climate sensitivity are uncertain, largely because of uncertainty in the long-term cloud feedback. I estimated the magnitude of the cloud feedback in response to short-term climate variations by analyzing the top-of-atmosphere radiation budget from March 2000 to February 2010. Over this period, the short-term cloud feedback had a magnitude of 0.54 ± 0.74 (2σ) watts per square meter per kelvin, meaning that it is likely positive. A small negative feedback is possible, but one large enough to cancel the climate’s positive feedbacks is not supported by these observations. Both long- and short-wave components of short-term cloud feedback are also likely positive. Calculations of short-term cloud feedback in climate models yield a similar feedback. I find no correlation in the models between the shortand long-term cloud feedbacks.
[1] Yang H, Li, X B. Cultivated land and food supply in China [J]. Land Use Policy, 2000, 17(2): 73-88. [2] Li Xiubin, Wang Xiuhong. Changes in agricultural land use in China: 1981 - 2000 [J]. Asian Geographer, 2003, 22(1-2):27-42. [3] MENG Ji-jun, FU Zai-yi. The research on the sustainable use of cultivated land resource in China. Areal Research and Development, 1998, 17(4):32-36. [4] LIU Cheng-wu, LI Xiu-bin. The changing characteristics of the agricultural land use intensity in China based on the production cost. Journal of Natural Resources, 2006, 21(1): 9-15. [5] ZHU Hui-yi, LI Xiu-bin, XIN Liang-jie. Intensity change in cultivated land use in China and its policy implications. Journal of Natural Resources, 2007, 22(6): 907-915. [6] LIU Cheng-wu, LI Xiu-bin. Regional differences in the changes of the agricultural land use in China during 1980-2002. Acta Geographica Sinica, 2006, 61(2): 139-145.
论文示例
http://www.nature.com/nature/journal/v468/n7325/full/nature09618.html#/references
http://www.sciencemag.org/content/330/6010/1523.full
Increased ice velocities in Greenland are contributing significantly to eustatic sea level rise. Faster ice flow has been associated with ice–ocean interactions in water-terminating outlet glaciers and with increased surface meltwater supply to the ice-sheet bed inland. Observed correlations between surface melt and ice acceleration have raised the possibility of a positive feedback in which surface melting and accelerated dynamic thinning reinforce one another, suggesting that overall warming could lead to accelerated mass loss. Here I show that it is not simply mean surface melt but an increase in water input variability that drives faster ice flow. Glacier sliding responds to melt indirectly through changes in basal water pressure, with observations showing that water under glaciers drains through channels at low pressure or through interconnected cavities at high pressure. Using a model that captures the dynamic switching between channel and cavity drainage modes, I show that channelization and glacier deceleration rather than acceleration occur above a critical rate of water flow. Higher rates of steady water supply can therefore suppress rather than enhance dynamic thinning, indicating that the melt/dynamic thinning feedback is not universally operational. Short-term increases in water input are, however, accommodated by the drainage system through temporary spikes in water pressure. It is these spikes that lead to ice acceleration, which is therefore driven by strong diurnal melt cycles and an increase in rain and surface lake drainage events rather than an increase in mean melt supply.