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The results obtained revealed that:(1) the Pacific yellowfin has larger ring-radii as well as scale size than the Indian Yellowfin;(2) the specimens from the western Indian have larger value in scale size and ring-radii than those from eastern Indian;(3) there is a significant difference in the estimated growth curves between male and female for the Pacific specimens, but not for the Indian specimens; and (4) it is convinced that there are two yellowfin groups in the Indian Ocean, viz., one concentrates in the western Indian and the other densely distributes in the waters around Sunda Islands and Banda Sea; intermingling of these two groups is supposed to be occurred around 100°E in the season of northern summer.
3李氏现象在太平洋和印度洋都很显著。(4)年轮每年形成二次，时间为2～4月及8～10月。(5)有关成长的parameters如下：太平洋K=0.386 L=174.9 t0=0.05 东印度洋 K=0.278 L=212.7 t0=-0.19 中印度洋 K=0.290 L=215.6 t0=-0.01 西印度洋 K=0.349 L=191.1 t0=0.06 (6)由钓获率的分布、体长组成和其他生物学资料及以往之结果加以综合分析，显示印度洋的黄鳍鲔可分为东、西两个族羣，一为以班达海和小巽他羣岛附近海域为中心的东方羣，另一则以西部印度洋赤道流域为中心的西方羣。此两羣在100°E附近发生混合交流。当北半球的夏天时，此混合交流的现象较为显著。
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For the climatic characteristics of the onset of the SCS summer monsoon, results reveal: 1 the SCS summer monsoon brusts at the 4th pentad in May; 2 the onset of the SCS summer monsoon is closely related to the southwesterly monsoon over the eastern Bay of Bengal, as induced by the intensification and eastward advancement of the latter; 3 the rainy season of the SCS summer monsoon bursts after the onset of the SCS summer monsoon basically; and 4 the atmospheric circulations exhibit rapid changes at different heights over the SCS and its adjacent districts, during the establishment peroid of the SCS summer monsoon, these include: i in lower troposphere, the southward expansion and deepening of the Indo-Burma trough; ii in middle troposphere, the rapid easterward retreat of the western Pacific subtropicl high form the SCS region, iii in upper troposphere, the fast radiation of the easterlies form the center of the SCS region to the whole of it apparently.
对于南海夏季风建立的气候特征，研究发现：(1)南海夏季风的建立具有爆发性，爆发的时间是5月第4候。(2)南海夏季风的建立与孟加拉湾东部西南季风有密切的关系，是孟加拉湾西南季风发展和东移的结果。(3)南海的夏季风雨季基本上是随着夏季风建立而建立的。(4)在南海夏季风建立期间，南海及其邻近地区高低空环流都有急速的变化，在对流层低层表现为印缅槽的南扩和加深，在对流层中层表现为西太平洋副热带高压迅速东移撤出南海地区，在对流层高层最明显的变化是东风带迅速地从南海中部向北扩展到整个南海地区。
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Difference of nitrogen competition and utilization in relay system Relay-planted with same late maturity or early maturity spring-sown maize, the yearly nitrogen absorption quantity of summer-sown late maturity maize YD 13 was highest, those of summer-sown middle maturity maize were middle, and those of summer-sown early maturity maize were lowest. While relay-planted with middle maturity, the yearly nitrogen absorption quantity of summer-sown late maturity maize YD13 was highest, those of summer-sown early maturity maize were middle, and those of summer-sown middle maturity maize were lowest.
不同熟期春夏玉米套作氮素竞争利用及其对产量和品质的影响 2.1 套作体系氮素竞争利用差异研究结果表明，与相同晚熟、早熟春玉米套作的夏晚熟品种YD13套作模式全年吸氮量均较高，其次是中熟品种，早熟品种全年吸氮量最低；而与中熟春玉米品种套作时，仍以夏晚熟品种YD13套作模式全年吸氮量最高，其次是早熟品种，中熟品种套作模式全年吸氮量最低。
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Indian summer：小阳春
是的,这是深秋,亦即北佬们所谓的"小阳春"(Indian Summer),下半年中最值得留恋的好天气. 不久寒流将从北极掠过加拿大的平原南侵,那便是戴皮帽、穿皮衣、着长统靴子在雪中挣扎的日子了. 而此刻,太阳正凝望平原上做着金色梦的玉蜀黍们;
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Indian summer：印地安的夏天
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Indian summer：春
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Indian Summer Rain：印地安夏雨
11 木星 Jupiter | 12 印地安夏雨 Indian Summer Rain | 13 晨光 Morning Air
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Indian Summer Rain：印度夏天的雨
17.Birds Over The Rainbow鸟儿飞越彩虹 | 18.Indian Summer Rain印度夏天的雨 | 01.One Day In Spring春日
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