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中国华南地区持续干期日数时空变化特征 总被引:1,自引:0,他引:1
利用华南地区46个地面气象站1960-2012年逐日降水数据,分析该地区各季节持续干期日数的时空分布特征。结果表明:1)近53年来,华南地区春季和夏季的持续干期日数呈波动下降趋势,下降速率分别为0.042和0.108 d·(10 a)-1;秋季和冬季的持续干期日数呈波动上升趋势,上升速率分别为1.911和0.118 d·(10 a)-1。广东省春季和夏季持续干期日数呈下降趋势,下降速率分别为0.171和0.243 d·(10 a)-1;秋季和冬季持续干期日数呈增加趋势,增加速率分别为1.737和0.32 d·(10 a)-1。广西省春、夏和秋季持续干期日数呈增加趋势,增加速率分别为0.109、0.046和2.117 d·(10 a)-1;冬季为减小趋势,减少速率为0.106 d·(10 a)-1。2)华南地区持续干期日数在春季呈从北向南逐渐增多的趋势,夏季呈自西南向东北逐渐增加的趋势,秋季呈自西向东逐渐增加的趋势,冬季呈从北向南逐渐增多的趋势。冬季的持续干期日数是4个季节中最长的,大致在20~44 d。3)华南地区春季持续干期日数变化倾向率在-1.20~1.00 d·(10 a)-1之间,增加趋势最明显的区域是广西省的南部地区,减少趋势最明显的区域是广东省的沿海地区;夏季在-1.00~0.60 d·(10 a)-1之间,呈增加趋势的区域主要位于广西省的中部和南部,呈减少趋势的区域位于广东省大部分地区和广西省的东部;秋季在0~3.50 d·(10 a)-1之间,整体呈现增加趋势,变化倾向率较大的区域主要位于广西省的中部和广东省的东北部沿海地区;冬季在-1.50~2.00 d·(10 a)-1之间,呈增加趋势的区域主要集中在广东省的中南部和东部地区,以及广西的东部边缘,呈减少趋势的区域主要集中在广东省的北部以及广西的中部和西北部地区。持续干期日数增加趋势最明显的季节是秋季。4)持续干期日数与降水量表现出负相关性,与气温和无降水日数表现为正相关性。降水量和无降水日数的变化对持续干期日数的变化起着重要的作用,而温度对持续干期日数的影响比较小。 相似文献
63.
The current risk management approach for the Norwegian offshore petroleum industry came into effect in 2001 and has been stable with minor changes for 15 years. Relatively few new installations were slated for development until quite recently, and several new projects have been started in the last few years. The paper considers the risk management approach in the pre-FEED phase and builds on two case studies selected from the most recent cases. These case studies have been evaluated with respect to how uncertainties are considered in the early phase, based on the submission of the Plan for Development and Operation, their evaluations by authorities and the supporting documents. Both case studies involve new concepts for which there is no experience from similar environments and/or water depths. In spite of what could have been expected, the case studies conclude that uncertainties have not been in focus at all during concept development. This appears to be definitely the case for the licensees, but also to be the case for the authorities. Some suggestions are presented for what could have been considered by the licensees and authorities. 相似文献
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Marcela González Cristina Dapeña Bibiana Cerne Odon Sánchez-Ccoyllo Saulo Freitas Pedro L. Silva Dias Héctor Panarello 《Environmental Fluid Mechanics》2009,9(4):409-425
The SALLJEX experiment was held during the summer 2002–2003. It consisted of three-dimensional observation of the atmosphere
to study the structure of the low level jet along the eastern slopes of the Andes. Daily precipitation water samples were
collected at two stations (Resistencia and Salta) in northern Argentina and isotope content was analyzed. The isotope data
were used in conjunction with air parcel trajectories obtained from a 3-D kinematic model (3D-MTC) developed by the University
of Sao Paulo, Brazil. Values of deuterium excess were related with air masses of continental origin, whilst low values were
associated with air masses with longer oceanic trajectories. Furthermore, although data are scarce, results show that oxygen-18
and deuterium excess in rainwater are related with the occurrence of the low level jet. 相似文献
66.
从保护臭氧层,保护环境的角度出发,介绍了氯氟烃化合物对环境的影响。阐述了用制冷剂R22代替R502在低蒸发温度应用时需要解决的问题和如何解决。 相似文献
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69.
Effects of solution conditions on the precipitation of phosphate for recovery. A thermodynamic evaluation 总被引:16,自引:0,他引:16
To understand the effects of solution conditions on the precipitation of calcium phosphates from wastewater for recovery, a computer programme PHREEQC was employed to calculate the speciation and saturation-index (SI) with respect to hydroxyapatite of a chemically defined precipitation system, which contains phosphate of 1–200 mg P/l, with Ca/P molar ratios of one to 10 times of the stoichiometric calcium to phosphorus molar ratio of hydroxyapatite, at a pH range of 7.0–11.0. The results show that the SI is respectively the logarithmic function of the phosphate concentration and the calcium concentration, increasing with the increase of either of them; the SI is a polynomial function of the solution pH value and increases with its increase, and the effect of solution pH value is due to its influence on base uptake of the precipitation reaction and the speciation of phosphate and calcium ions; the SI is also a logarithmic function of the solution ionic strength but decreases with its increase; at the temperature range of 5–30 °C the SI increases linearly with solution temperature and the effect of temperature is also due to its influence on the speciation of phosphate and calcium ions. 相似文献
70.