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The precipitation only has faintish negative correlations with N concentrations (p〉 0.05), but the NH^+ 4-N has significant positive correlations with NO^- 3-N and TON (p〈 0.05), and they might have homologue.

结果表明,各形态氮月均浓度之间差别较大,具有明显的季节性,原因主要与人类活动、降水强度及频次、风向、地理位置以及氮氧化物自然排放有关;湿沉降的TN组成以TIN为主(51.38%-98.96%),TIN又以NH^+ 4-N和NO^- 3-N特别是NH^+ 4-N为主,降水天气系统的路径在很大程度上影响着降水中各形态氮的组成;降水量与各形态氮浓度均呈较弱的负相关(P〉0.05),而NH^+ 4-N与NO^- 3-N、TON均呈显著正相关(P〈0.05),它们可能具有同源性。

The canopy of the species is strong in obstructing storms and reducing soil surface erosion and the water-holding capacity.As a result,the surface erosion is less than that on the grassed slope by 11%;the litter under the canopy has a depth of 5.5 cm on the average;and each adult tree can hold 0.3~0.69 m3 of rainfall.

杨梅树冠和树形有极强的阻截暴雨,减少地表径流以及蓄水能力,地表径流比草坡减少11%,树冠下部凋落物平均厚度5.5 cm,每株成年树可保存0.30~0.69 m3的降水量

The authors collect and process the discharge rate data of Hongshanzui hygrometric station from 1956 to 2003,day-to-day precipitation and air temperature data of Shihezi City from 1953 to 2003.The correlation curves of the three variables are constructed.And the functions of annual precipitation and mean annual air temperature,to mean annual flow rate of Manas River are analyzed.

笔者对玛纳斯河出山口红山嘴水文站的流量资料(1956—2003年)及石河子市的逐日降水和气温资料(1953—2003年)进行分析,介绍各自变化特点并建立它们之间的年均变化对比曲线,分析年均流量与年降水量和年均气温的关系。

The effect of topography on precipitation can be extract from the precipitation.Secondly, considering the incontinuity of the precipitation distributing, we use improved the Stepwise Interpolation Approach, SIA, to combine with the multi-variable successive regression equations.

其次,充分考虑到降水分布的不连续性,利用逐步插值方法与多元回归方程结合,不但取得了与事实相符的计算结果,而且显著地提高了年降水量空间分布的计算精度。

Altitude the precipitation gradient of 3000 meters of above may fluctuate somewhat, year of fall that Dan Xue line takes is likely amount to 3000 millimeter, still present increscent trend.

海拔3000米以上的降水梯度可能有所波动,但雪线带的年降水量可能达3000毫米,仍呈现增大的趋势。

The resultsshow that the Pliocene paleoclimate of Tuantian Basin is characterized by the mean annualtemperature 21.3-25.1℃, mean temperature of the warmest month21.3-25.1℃, mean temperature of the coldest month 10.8-14.6℃, difference intemperature between the coldest and warmest month 11.3-16.3℃, mean annualprecipitation 1225.7-1638.3 mm, and relative humidity 75-82%.

通过共存因子分析法,取团田植物群37个化石种的最近亲缘种的气候因子的共存区间,定量重建了团田晚上新世的古气候特征:年均温为16.4-19.8℃,最热月平均气温21.3-25.1℃,最冷月平均气温10.8-14.6℃,气温年较差11.3-16.3℃,年均降水量1225.7-1638.3 mm,年均相对湿度75-82%。

The effects of meterological factors on the growth quantity of Larix leptolepis were different analyzed by step-by-step regression and correlation coefficient analysis.

采用多元逐步回归方法和关联分析法得出的气候因素对日本落叶松生长量影响的排序次序是有差异的,但基本结论具有共同性:影响重要的气象因子不管是上年夏季的降水量,还是上年9~10月相对湿度都与降水有关,表明该地区日本落叶松生长量与降水状况和春季地温有密切关系。

The increment of height Larix leptolepis was affected mainly by precipitation of last summer, and volume increment was affected mainly by the precipitation of last summer and 10 cm groud temperature of last spring.

由此可以综合得出对日本落叶松生长量影响较大的气象因子是上年夏季的降水量和春季10cm地温。

Manas River to the west, more precipitation, most of the grassland and marshes.

玛纳斯河以西,降水量较多,大部分为草原和沼泽地带。

After that wet zenith delay is calculated into PWV, and field meteorologic data are combined to analyzing.

从两站的历史气象资料出发,通过回归计算得到适合两站 1、2月份的转换系数K ;然后进行天顶湿延迟至可降水量的转换,结合现场的气象资料进行对比分析。

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