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1.Strawberries grow best in cool,moist climate.
草莓在阴凉潮湿气候 中生长最佳.收藏指正
2.Strawberries grow best in a cool, moist climate.
草莓最适于在凉爽、潮湿气候条件下生长。收藏指正
3.Two layers of dark colored mudstones 10~20 m thick were found in Sushanhe Formation, which suggests that a short period of moist climate occurred during Cretaceous when the climate was mainly dry in the area.
在苏善组的 2个层位发现了厚度达 10~ 2 0m的暗色泥岩 ,反映本区白垩纪的干热型气候曾间歇性出现过短暂的潮湿时期收藏指正
4.The loess features appear mainly wind phase with the wind--water two phases by calculating grain size prameters and analysing the grain--size. The high content of clay(<5 μm), with the average of 54.32%, and mulistory calcareous loess layers indicate that it is formed in the condition of moist climate, dominating summer monsoon.
对粒度参数的计算和粒度成分的分析表明,该套黄土显示风成相为主,具有风水两相的特点,黏粒(<5μm)含量很高,平均含量54 32%,具有多层钙结黄土层,揭示出该套黄土形成于气候相对湿润,且以夏季风为主,风化成壤作用很强的环境中。收藏指正
5.They have survived the destructive influences of man through their location in precipitous topography and the moist winter micro-climate.
由于峡谷地势峻峭,加上冬季仍保持潮湿,故林木得以保存,未受人为破坏。收藏指正
6.By using various oxide ratios in argillite, the paper discussed the situation of Paleoclimate and its evolutioary law from Carboniferous to Jurassic Period in Shanganning Basin. From Mid - Carboniferous to mid - Triassicepoch and late Triassic epoch to Antinian, the ratios of various oxides in argillite show two unsimilar cycles which gradually increase or decrease in vertical profile,accordingly, during the same period the paleoclimate exists the early and late two cycles i. e. from the moist to semimoist and semiarid climate.
应用泥质岩的多种氧化物比值,探讨了陕甘宁盆地石炭至侏罗纪的古气候状况及其演变规律,自中石炭世至中三叠世,再由晚三叠世至安定期,泥质岩的各种氧化物比值有着逐渐依次增大或减小的两个互不雷同的旋回,与之相应,以上时期反映在古气候上存在着由潮湿→半潮湿→半干燥的早、晚两个旋回。收藏指正
7.during 3.75-3.47 Ma the vegetation belonged to mountainous,warm-temperate,mixed needleleaf and broadleaf forest and the climate changed from cool-dry to warm-moist;
3.75~3.47 Ma时期,属于山地暖温带针阔叶混交林,气候由温凉干旱向温暖湿润过渡;收藏指正
8.The main conclusions are as follow:1. During the past nearly 50 years, the increase rate of precipitation and evapotranspiration is 0.557mm/a and 0.132mm/a, so the climate of Dari changed from drought to moist.
(1) 近50a来达日县降水年增加率为0.557mm/a,而该县最大可能蒸散发量的年增加率为0.132mm/a,气候总体趋势是由干旱向湿润方向发生转变;收藏指正
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