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“风的形成”教具的改进与创新 被引量:1
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作者 蔡世娟 《实验教学与仪器》 2023年第8期65-66,共2页
“风的形成”是人教版物理八年级上册第六章第四节的教学内容。教材实验设计以酒精灯、纸风车、细线为器材模拟“风的形成”,但此实验存在设计不严谨、安全性较低、不易操作、实验现象不明显等诸多不足。为此,自制创新教具对教材实验进... “风的形成”是人教版物理八年级上册第六章第四节的教学内容。教材实验设计以酒精灯、纸风车、细线为器材模拟“风的形成”,但此实验存在设计不严谨、安全性较低、不易操作、实验现象不明显等诸多不足。为此,自制创新教具对教材实验进行改进,改进后的实验设计更科学、探究性更强、现象更直观,更好地发挥了演示实验在物理教学中的作用。 展开更多
关键词 风的形成 演示实验 自制教具 改进
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从模拟走向真实的科学概念建构之路
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作者 吴小兵 俞灵 《新课程》 2017年第4期12-13,共2页
模拟是根据研究对象的本质特性,建立或选择一种与研究对象类似的模型,借助模型进行实验研究,不仅可以把学生陌生的、抽象的事物转化为学生熟悉的、直观的模型,使概念具体化、形象化,也可以帮助学生更直观、更深刻地把握研究对象的... 模拟是根据研究对象的本质特性,建立或选择一种与研究对象类似的模型,借助模型进行实验研究,不仅可以把学生陌生的、抽象的事物转化为学生熟悉的、直观的模型,使概念具体化、形象化,也可以帮助学生更直观、更深刻地把握研究对象的本质和特征。以《风的形成》为例,针对实际教学中模拟实验存在的问题,引领学生从模拟走向真实,主动建构起风的形成的科学概念。 展开更多
关键词 模拟实验 科学概念 风的形成
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让学生与实验仪器携手成为朋友
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作者 郑建丽 《教学仪器与实验》 2011年第6期55-57,共3页
“风的形成演示箱”为《风的成因》一课中学生进行主动探究活动所依托的主要实验仪器。教师为学生创造学习情境,让学生成为课堂的主人,在一系列的思考与探究活动中,携手“风的形成演示箱”,进而获得“风的成因”的科学概念。并在此... “风的形成演示箱”为《风的成因》一课中学生进行主动探究活动所依托的主要实验仪器。教师为学生创造学习情境,让学生成为课堂的主人,在一系列的思考与探究活动中,携手“风的形成演示箱”,进而获得“风的成因”的科学概念。并在此过程中培养学生的科学探究能力和实验精神。 展开更多
关键词 实验仪器 科学探究 风的形成演示箱
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CONTRAST ANALYSIS OF APRIL TYPHOONS LEO AND NEOGURI
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作者 卢山 吴乃庚 《Journal of Tropical Meteorology》 SCIE 2011年第4期409-417,共9页
The conventional observations data,NCAR/NCEP-2 reanalysis data,and NOAA outgoing longwave radiation data are used to investigate different characteristics of Leo and Neoguri,two April typhoons that ever made landfall ... The conventional observations data,NCAR/NCEP-2 reanalysis data,and NOAA outgoing longwave radiation data are used to investigate different characteristics of Leo and Neoguri,two April typhoons that ever made landfall on the continent of China over the past 60 years.The results showed that both Leo and Neoguri occurred during the La Nina events.Strong convective activity,weak vertical wind shear and upper-level divergence were in favor of the formation of these April typhoons.Leo originated from a monsoon depression and Neoguri evolved from an easterly wave.The meandering moving track of Leo attributed to strong northeast monsoon and a weak and changeable subtropical high;the steady moving track of Neoguri was governed by a strong and stable subtropical high.Leo and Neoguri had similar terrain conditions and intensities during landfall but were different in precipitation as water vapor transport and duration of kinetic uplifting resulted in apparent discrepancies between them. 展开更多
关键词 April typhoons formation mechanisms moving track typhoon precipitation
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PRELIMINARY STUDY ON RELATIONSHIP BETWEEN DOUBLE VORTICES SELF-ORGANIZATION AND TYPHOON FORMATION IN BAROCLINIC ENVIRONMENT
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作者 滕代高 罗哲贤 +1 位作者 潘劲松 余晖 《Journal of Tropical Meteorology》 SCIE 2010年第4期372-379,共8页
The relationship between the self-organization of double vortices (SODVs) and the formation of typhoons was discussed based on six numerical experiments with the Fifth-Generation National Center for Atmospheric Rese... The relationship between the self-organization of double vortices (SODVs) and the formation of typhoons was discussed based on six numerical experiments with the Fifth-Generation National Center for Atmospheric Research/Penn State Mesoscale Model (MM5) and further discussion was made with a real typhoon case. The results showed that there is a critical distance dc for SODVs in baroclinic atmosphere. When the distance between separated vortices is smaller than or equal to d~, the double vortices self-organize into a typhoon-like vortex with two spiral bands. But the double vortices cannot have such organization if the distance between them is larger than de. The value of dc is about 380 km in the context of ideal conditions in this paper, larger than that achieved in a barotropic model. A typical typhoon case in 2005 (Haitang) was selected to verify the above-mentioned conclusions. It was found that the SODV is one of the important and typical ways for the formation of typhoons. 展开更多
关键词 baroclinic atmosphere self-organization of double vortices typhoon formation
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COMPARISON STUDY ON THE INTRASEASONAL VARIATIONS IN CIRCULATIONS AND PRECIPITATION MODULATED BY THE TROPICAL CYCLOGENESIS OVER SOUTH CHINA SEA-WESTERN PACIFIC DURING GUANGDONG FLOODING PERIOD
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作者 李春晖 万齐林 +2 位作者 郑彬 谷德军 林爱兰 《Journal of Tropical Meteorology》 SCIE 2011年第4期363-374,共12页
Based on tropical cyclone datasets from Shanghai Typhoon Institute of China Meteorological Administration,the National Centers for Environmental Prediction (NCEP,USA) reanalysis data and the rainfall records from 743 ... Based on tropical cyclone datasets from Shanghai Typhoon Institute of China Meteorological Administration,the National Centers for Environmental Prediction (NCEP,USA) reanalysis data and the rainfall records from 743 stations in China,the impacts of cyclogenesis number over the South China Sea and the western Pacific are studied on the 30-60-day oscillations in the precipitation of Guangdong during the flooding period.The year with more-than-normal (less-than-normal) tropical cyclogenesis is defined as a 'high year' ('low year').In light of the irregular periodic oscillations,the method used to construct the composite life cycle is based on nine consecutive phases in each of the cycles.Phases 1,3,5,and 7 correspond to,respectively,the time when precipitation anomalies reach theminimum,a positive transition (negative-turning-to-positive) phase,the maximum,and a negative transition phase.The results showed that the precipitation of the 30-60-day oscillations is associated with the interaction between a well-organized eastward propagation system from the Arabian Sea/Bay of Bengal and a westward-propagating system (with cyclonic and anticyclonic anomalies in the northwest-southeast direction) from the South China Sea to western Pacific during the high years,whereas the precipitation is affected during a low year by the circulation over the South China Sea and western Pacific (with cyclonic and anticyclonic anomalies in the northeast-southwest direction).During the high year,the warm and wet air mass from the ocean to the west and south are transported to Guangdong by westerly anomalies and an enclosed latitudinal cell,which ascends in the Northern Hemisphere low latitudes and descends in the Southern Hemisphere low latitudes.During the low year,the warm and wet air mass from the ocean to the south is transported to Guangdong by southwesterly wind anomalies and local ascending movements.Because the kinetic energy,westerly,easterly shift,vertical velocity and vapor transportation averaged over (109-119° E,10-20° N) is stronger in high years than those in low years,the precipitation of the 30-60-day oscillations in Guangdong is higher in high years than that in low years. 展开更多
关键词 cyclogenesis number over the South China Sea and western Pacific precipitation in Guangdong province 30-60-day oscillation
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