共查询到20条相似文献,搜索用时 187 毫秒
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《南京气象学院学报》1995,(4)
TOGACD-ROM资料介绍(续)国家自然科学基金委员会地球科学部南京气象学院大气资料服务中心资料通讯第2卷第4期(总第7期)1995年10月4GEOSAr海面高度资料这些资料由NOAANationalService提供。原始资料是GEOSAT(Ge... 相似文献
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《南京气象学院学报》1997,(4)
资料通讯国家自然科学基金委员会地球科学部南京气象学院大气资料服务中心第4卷第1期(总第10期)1997年12月ECMWF数值模拟资料CD┐ROM和CMAP降水资料介绍1ECMWFCD┐ROM这些CD-ROM上存放着选自ECMWF(欧洲中期预报中心)“... 相似文献
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用NOAA/AVHRR资料遥感土壤水分时风速的影响 总被引:12,自引:1,他引:11
以热惯量法为基础,在地理信息系统(GIS)的支持下,通过计算地形参数R与F,间接考虑了风速对用NOOAA/AVHRR资料遥感土壤水分的影响。结果表明:考虑风速后,遥感土壤水分的精度比热惯量法有所提高;风速对遥感土壤水分的影响主要限于土壤浅层,到30cm深度以下时可以不考虑其影响;遥感土壤水分的最佳深度并不在土壤表层,而在20cm深度左右。 相似文献
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丁一汇 《中国气象科学研究院年报》1996,(1)
SCIENTIFIC-OPERATIONALEXPERIMENTSANDSYNOPTIC-DYNAMICSTUDYOFHEAVYRAINFALLS¥DingYihui(丁一汇)SCIENTIFIC-OPERATIONALEXPERIMENTSANDS... 相似文献
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《中国气象科学研究院年报》1994,(1)
ESTIMATIONOFVERTICALWINDFIELDFROMSINGLE-DOPPLERRADARRHIOBSERVATIONSPengHong(彭红)andGeRunsheng(葛润生)InstituteofMesoscaleMeteorol... 相似文献
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《中国气象科学研究院年报》1994,(1)
ANUMERICALEXPERIMENTONTHEINFLUENCESOFTHEQINGHAI-XIZANGPLATEAUONTHEUPSTREAMBLOCKINGEVENTZhengQinglin(郑庆林),GuYu(古瑜),SongQingli(... 相似文献
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Based on the data of monthly mean air temperature and precipitation from about 400 stationsin 1951—1995.and the data of maximum and minimum air temperatures,relative humidity,totalcloud cover and low-cloud cover,sunshine duration,evaporation,wind speed,snow-covered daysand depth,and soil temperatures in 8 layers from 0 m down to 3.2 m from 200 odd stations in 1961—1995.the climate change and its characteristics in China in recent 45 years have been analyzedand studied comprehensively.This paper,as the first part of the work.has analyzed the climatechange and regularities of such meteorological elements as mean air temperature,maximum andminimum air temperatures,precipitation,relative humidity and sunshine duration.The possiblemechanism on climate change in China and the climate change and regularities of othermeteorological elements will be discussed in another paper as the second part. 相似文献
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以简化农田实际蒸散的计算过程为目的,利用1999年河北定兴县中国气象科学研究院农业气象试验基地的玉米田0~300 cm土壤湿度和气象要素的实测资料以及华北地区5个站1991~1995年0~50 cm土壤湿度和气象资料,探讨由简化参考蒸散模式计算玉米田实际蒸散的可能性;对比了Priestley-Taylor模式和FAO(1998)Penman-Menteith模式的计算结果,以农田试验资料为基础,采用叶面积系数和平均土壤相对湿度为因子,建立了实际蒸散的计算模式。并以华北地区8个站1999~2000年0~50 cm土壤湿度和气象资料进行验证,平均误差一般为10%~15%. 相似文献
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CoLM模式对青藏高原中部BJ站陆面过程的数值模拟 总被引:8,自引:2,他引:6
利用公共陆面模式Common Land Model(CoLM)及"全球协调加强观测计划之亚澳季风青藏高原试验"(CAMP/Tibet)中那曲地区Bujiao(BJ)站2002—2004年的观测资料对该地区进行了单点数值模拟试验。通过比较模拟与观测的地表能量通量,表明CoLM较成功地模拟了该地区的能量分配。模式对向上的短波辐射、向上的长波辐射、净辐射及土壤热通量模拟得较好,但冬季存在偏差。进一步比较了模拟和观测的土壤温度及土壤湿度,发现浅层60 cm土壤温度模拟较好,深层存在偏差,表现为土壤温度变化滞后于实际变化。土壤湿度总体偏小,尤其是冬季冻结期,土壤冻融过程中忽略了土壤液态水在温度0℃以下仍能存在,含冰量模拟偏高。 相似文献
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Summary ?This paper deals with variations and trends in some components of the water balance: the soil water content; evaporation
loss from the soil (from the surface and underlying layers); transpiration; ground water recharge and runoff. These components
are calculated by means of the Palmer procedure. This analysis is based on data from Osijek, Croatia from this century (1900–1995).
Besides the meteorological input parameters necessary for the water balance calculations, i.e. precipitation, temperature
and relative humidity, the pedological characteristics of this area have also been taken into account. Fluctuations have been
considered by means of the 11-year binomial filtered series and linear trends were tested by means of the Mann-Kendall rank
test. For a closer look on the trends of water balance components, a progressive analysis of the time series was performed,
too. The results show a significant increase in potential evapotranspiration and evapotranspiration and decrease in runoff
and soil water content has occurred during the century.
Received February 22, 1999/Revised August 3, 1999 相似文献
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文中分析了庆阳地区春季降水气候特征和环流形势 ,用 1995~ 1998年 3~ 5月T10 6资料建立了该区 8县 (市 )春季降水、温度MOS预报方程 ,进行了回代检验和试报 ,并提出了模式更换后的处理方法 相似文献
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近20年华北地区土壤水储量变化趋势及水分管理与调配对策 总被引:7,自引:1,他引:6
从35个台站土壤湿度实测资料出发,探讨了近20年华北地区土壤水储量变化趋势及时空特征。结果表明:全区年平均0~50 cm土壤水储量总体呈减少趋势,但区域差异明显。土壤变干最显著的两个中心区域分别为京津塘地区和山西西部,次显著中心为内蒙古东部。在0~50 cm深度范围内,从地表面开始,随深度增加,土壤水储量的减少幅度逐渐增加,且季节特征明显,即春秋季减少幅度大于夏冬季。各分区土壤水储量的变化趋势呈现出显著的年代际特征,就0~50 cm土壤水储量而言,各分区存在一个共同特点:1995~2002年均呈明显的波动下降变化趋势。土壤变干的趋势,对华北地区农业和生态具有一定的不利影响,因此结合区域实际提出相应的水分管理与调配措施。 相似文献
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《大气与海洋》2013,51(1):79-97
Abstract Mackenzie River discharge was at a record low in water year (WY) 1995 (October 1994 to September 1995), was near average in WY 1996, and was at a record high in WY 1997. The record high discharge in WY 1997, with above average flow each month, was followed by a record high flow in May 1998, then a sharp decline. Through diagnosing these changing flows and their expression in the Beaufort Sea via synthesis of observations and model output, this study provides insight into the nature of the Arctic's freshwater system. The low discharge in WY 1995 manifests negative anomalies in P‐E and precipitation, recycled summer precipitation, and dry surface conditions immediately prior to the water year. The complex hydrograph for WY 1996 reflects a combination of spring soil moisture recharge, buffering by rising lake levels, positive P‐E anomalies in summer, and a massive release of water held in storage by Bennett Dam. The record high discharge in WY 1997 manifests the dual effects of reduced buffering by lakes and positive P‐E anomalies for most of the year. With reduced buffering, only modest P‐E the following spring led to a record discharge in May 1998. As simulated with a coupled ice‐ocean model, the record low discharge in WY 1995 contributed to a negative freshwater anomaly on the Mackenzie shelf lasting throughout the winter of 1995/96. High discharge from July–October 1996 contributed approximately 20% to a positive freshwater anomaly forming in the Beaufort Sea in the autumn of that year. The remainder was associated with reduced autumn/winter ice growth, strong ice melt the previous summer, and positive P‐E anomalies over the ocean itself. Starting in autumn 1997 and throughout 1998, the upper ocean became more saline owing to sea‐ice growth. 相似文献
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