黑龙江省气候成因

黑龙江省的气候，是在众多的相关地理要素共同作用下形成的，本文从纬度位置、季风环流和地形因素3个主要方面进行了分析．而且，在分析其对气候形成的影响时，涉及的气候要素主要是气温和降水．纬度位置对气候的影响，主要体现在热量条件上．季风环流从气温和降水两个方面影响黑龙江省气候．地形因素干扰、破坏着上述两种因素所形成的规律，在一定程度上隔断了气候要素经向和纬向的空间地带性分布，从而使气候变得更为复杂。     

天水半湿润山区绿化气候及适生林草区划研究

通过20世纪70~90年代30年气象资料统计分析,建立了天水半湿润山区适生林草区划数学模型;通过量化计算,得出了区内不同区域水、热匹配指标,并进行了适生林草配置的四级农业气候区划,为该区生态环境建设提供了科学依据.     

科技团体创造力评估模型研究

本文依据创造心理学范式,论述了关于科技团体创造力评估模型的理论探索、实证研究和模型建构的问题.所建构模型对于我国各级各类科研管理决策层预测和检验科技团体创造力水平以提高管理科学性,具有一定实用意义.     

全球气候治理格局下中国低碳技术的发展取向研究

本文主要通过文献研究、政策调研的方法,梳理了中国参与全球气候治理下的低碳技术发展形势。研究发现,中国未来面临的减排压力较大,发展低碳技术势在必行。但是,由于受国际经济利益博弈格局的影响,以及贸易保护主义盛行,实际低碳技术转移效果很差,未来也很难实现突破,所以发展自主研发的低碳技术产业是我国未来的发展方向。中国应积极提升低碳技术专利质量、完善研发模式并实现技术的知识产权战略布局。     

Butterflies (Lepidoptera: Papilionoidea) of Mount Kilimanjaro: Nymphalidae subfamilies Libytheinae,Danainae, Satyrinae and Charaxinae

This paper, which presents an annotated checklist of the ‘lower Nymphalidae’ (Libytheinae, Danainae, Satyrinae, Charaxinae), is the fourth in a series on the butterfly fauna of Mount Kilimanjaro. Four genera of lower Nymphalidae (Danaus, Amauris, Bicyclus, Charaxes), with a total of 11 included species, are known or believed to occur within the main forest zone, from c. 1800 to 2800 m. Of these, only three species of Charaxes (Charaxes berkeleyi, Charaxes ansorgei, Charaxes xiphares) may be restricted locally to this primary forest. The lower slopes fauna, below 1800 m, is considerably richer, with a total of 11 genera and 41 species listed (8 species of which extend into the forest zone). Possible additional species, dubious earlier records, problems with African subspecies of Danaus chrysippus, a need for more work on certain Satyrinae, and classification of the genus Charaxes are discussed. An identification key to the subfamilies of Nymphalidae, and the 19 genera of Libytheinae, Danainae, Satyrinae, Charaxinae that occur in Tanzania, together with a key to the adults of all the species of these four subfamilies considered to occur or have occurred on Kilimanjaro, with 206 colour images, are included as online Supplementary Information.     

Sea surface temperature records of core ZY2 from the central mud area in the South Yellow Sea during last 6200 years and related effect of the Yellow Sea Warm Current

Sea surface temperature (SST) records in the South Yellow Sea during the last 6200 years are reconstructed by the unsaturation index of long-chain alkenones (K 37 U ’) in sediment core ZY2 from the central mud area.The SST records varied between 14.1 and 16.5°C (15.6°C on average),with 3 phases:(1) A high SST phase at 6.2-5.9 cal ka BP;(2) A low and intensely fluctuating SST phase at 5.9-2.3 cal ka BP;and (3) A high and stable SST phase since 2.3 cal ka BP.Variation of the SST records is similar to intensity of the Kuroshio Current (KC),and corresponds well in time to global cold climate events.However,the amplitude of the SST response to cooling events was significantly different in different phases.The SST response to global cooling event was weak while the KC was strong;and the SST response was strong while the KC was weak.The difference in amplitude of the SST response is possibly caused by the modulation effect of the Yellow Sea Warm Current which acts as a shelf branch of the KC and a compensating current induced by the East Asia winter monsoon.The warm waters brought by the Yellow Sea Warm Current cushion the SST decrease induced by climate cooling,and both the Kuroshio and East Asian winter monsoon play important roles in the modulation mechanism.The SST records display a periodicity of 1482 years.The same period was found in the KC records,indicating that variation of the SST records in the central South Yellow Sea is strongly affected by KC intensity.The same period was also found in Greenland ice cores and North Atlantic and Arabian Sea sediment cores,showing a regional response of marine environmental variability in the East China Seas to that in the global oceans.     

Forced response of atmospheric oscillations during the last millennium simulated by a climate system model

Variations in global atmospheric oscillations during the last millennium are simulated using the climate system model FGOALS_gl. The model was driven by reconstructions of both natural forcing (solar variability and volcanic aerosol) and anthropogenic forcing (greenhouse gases and sulfate aerosol). The model results are compared against proxy reconstruction data. The reconstructed North Atlantic Oscillation (NAO) was out of phase with the Pacific Decadal Oscillation (PDO) in the last millennium. During the ...     

The methodology of quantitative assess economic output of climate change

A method is introduced in this paper to study the effect of future climatic change on the economy. The researchers determine the economic output of climate change from historical data, and provide a method to quantitatively predict economic output of climate change by an economic-climatic model. A historical reciprocating examination is used to analyze output data for various crops in eight agricultural areas in China and meteorological data from 160 observatories in China from 1980 to 2000. The results show that the methods used are reasonable to a certain extent and good in application.     

Changes in physical features of Glacier No. 1 of the Tianshan Mountains in response to climate change

This study analyzes the changes in glacier zones and snow composition of Glacier No.1 in the Tianshan Mountains of China since 1961,and their possible relations with climate.It is found that precipitation dominated the snow composition and that air temperature and precipitation controlled the distribution of glacier zones,but interannual change in precipitation had a relatively large effect on glacier zones and snow composition during 1963–1981 (P10) and 1963–1989 (P11).However,during 1982–2007 (P20) and 19...     

楚雄市气候变化及对水资源的影响

利用楚雄市1961～2010年50 a的气候和水资源等资料,分析了楚雄市近半个世纪以来气候的变化及其对径流、水资源变化的影响.分析结果表明:50 a来楚雄市各季和年平均气温均呈上升趋势,年平均气温以0.33℃/10 a速率上升,冬季平均气温增暖速率最为显著;近50 a来楚雄市年降水量有增多的趋势,以21.26mm/10 a的速度在递增.春季和夏季降水量增加较多;而冬季和秋季平均降水量则呈缓慢增多的趋势.水资源总量、地表水径流量、地下水呈减少趋势.