根据作者提出的 Ca CO3淀积深度理论、风化剖面的野外鉴别和室内 Ca CO3、磁化率测定、粒度分析 ,确定了陕西长武第 4、第5层古土壤底部之下存在深部风化黄土层和迁出了土壤层的 Ca CO3结核层。这种风化黄土层和 Ca CO3淀积层的发育表...根据作者提出的 Ca CO3淀积深度理论、风化剖面的野外鉴别和室内 Ca CO3、磁化率测定、粒度分析 ,确定了陕西长武第 4、第5层古土壤底部之下存在深部风化黄土层和迁出了土壤层的 Ca CO3结核层。这种风化黄土层和 Ca CO3淀积层的发育表明当时风化淋滤作用超出了成壤带深度范围 ,指示长武第 4、第 5层古土壤为不具 Ca CO3淀积层的中酸性、淋溶型森林土壤。该风化层代表了降水丰富的气候事件 ,当时年均降水量为 90 0 mm左右。展开更多
To accurately evaluate the carbon sequestration potential and better elucidate the relationship between the carbon cycle and regional climate change, using eddy covariance system, we conducted a long-term measurement ...To accurately evaluate the carbon sequestration potential and better elucidate the relationship between the carbon cycle and regional climate change, using eddy covariance system, we conducted a long-term measurement of CO 2 fluxes in the rain-fed winter wheat field of the Chinese Loess Plateau. The results showed that the annual net ecosystem CO 2 exchange （NEE） was （-71.6±5.7） and （-65.3±5.3） g C m-2 y-1 for 2008-2009 and 2009-2010 crop years, respectively, suggesting that the agro-ecosystem was a carbon sink （117.4-126.2 g C m-2 yr-1）. However, after considering the harvested grain, the agro- ecosystem turned into a moderate carbon source. The variations in NEE and ecosystem respiration （R eco ） were sensitive to changes in soil water content （SWC）. When SWC ranged form 0.15 to 0.21 m3 m-3, we found a highly significant relationship between NEE and photosynthetically active radiation （PAR）, and a highly significant relationship between R eco and soil temperature （T s ）. However, the highly significant relationships were not observed when SWC was outside the range of 0.15-0.21 m3 m-3. Further, in spring, the R eco instantly responded to a rapid increase in SWC after effective rainfall events, which could induce 2 to 4-fold increase in daily R eco , whereas the R eco was also inhibited by heavy summer rainfall when soils were saturated. Accumulated R eco in summer fallow period decreased carbon fixed in growing season by 16- 25%, indicating that the period imposed negative impacts on annual carbon sequestration.展开更多
利用南京大学浦口校区大气科学园的近地层湍流脉动资料及Meteorological InformationComprehensive Analysis and Process System气象数据资料,针对2008年5月南京地区一次降水过程,分析比较了降水前后的湍流强度、归一化湍流动能、近地...利用南京大学浦口校区大气科学园的近地层湍流脉动资料及Meteorological InformationComprehensive Analysis and Process System气象数据资料,针对2008年5月南京地区一次降水过程,分析比较了降水前后的湍流强度、归一化湍流动能、近地层通量输送和速度能谱特征.结果表明:从气象要素上看,降水临近时风速变化大,温度、气压降低明显,降水期间湿度很高.从湍流特征上看,降水时湍流强度突变增大,归一化湍流动能也变大,湍流活动增强;u、v方向动量输送-u′w′、-v′w′强度都增大,但输送方向相反,此时近地层归一化摩擦速度也明显变大;感热通量w′T′迅速减小,甚至微弱逆向输送;降水前后风速能谱惯性副区基本满足Kolmogorov的-2/3次方律,降水时u、v能谱低频段峰值频率左移明显,分析低频段峰值对应涡的尺度发现,近地层中降水前后贡献湍流能量最大的涡尺度存在很大差异.展开更多
Quantitative precipitation estimation and rainfall monitoring based on meteorological data, potentially provides continuous, high-resolution and large-coverage data, are of high practical use: Think of hydrogeological...Quantitative precipitation estimation and rainfall monitoring based on meteorological data, potentially provides continuous, high-resolution and large-coverage data, are of high practical use: Think of hydrogeological risk management, hydroelectric power, road and tourism. Both conventional long-range radars and rain-gauges suffer from measurement errors and difficulties in precipitation estimation. For efficient monitoring operation of localized rain events of limited extension and of small basins of interest, an unrealistic extremely dense rain gauge network should be needed. Alternatively C-band or S-band meteorological long range radars are able to monitor rain fields over wide areas, however with not enough space and time resolution, and with high purchase and maintenance costs. Short-range X-band radars for rain monitoring can be a valid compromise solution between the two more common rain measurement and observation instruments. Lots of scientific efforts have already focused on radar-gauge adjustment and quantitative precipitation estimation in order to improve the radar measurement techniques. After some considerations about long range radars and gauge network, this paper presents instead some examples of how X-band mini radars can be very useful for the observation of rainfall events and how they can integrate and supplement long range radars and rain gauge networks. Three case studies are presented: A very localized and intense event, a rainfall event with high temporal and spatial variability and the employ of X-band mini radar in a mountainous region with narrow valleys. The adaptability of such radar devoted to monitor rain is demonstrated.展开更多
The detailed analysis of individual rain events characteristics is an essential step for improving our understanding of variation in precipitation over different topographies. In this study, the homogeneity among rain...The detailed analysis of individual rain events characteristics is an essential step for improving our understanding of variation in precipitation over different topographies. In this study, the homogeneity among rain gauges was investigated using the concept of “rain event properties,” linking them to the main atmospheric system that affects the rainfall in the region. For this, eight properties of more than 23,000 rain events recorded at 47 meteorological stations in Mumbai, India, were analyzed utilizing seasonal (June-September) rainfall records over 2006-2016. The high similarities among the properties indicated the similarities among the rain gauges. Furthermore, similar rain gauges were distinguished, investigated and characterized by cluster analysis using self-organizing maps (SOM). The cluster analysis results show six clusters of similarly behaving rain gauges, where each cluster addresses one isolated class of variables for the rain gauge. Additionally, the clusters confirm the spatial variation of rainfall caused by the complex topography of Mumbai, comprising the flatland near the Arabian Sea, high-rise buildings (urban area) and mountain and hills areas (Sanjay Gandhi National Park located in the northern part of Mumbai).展开更多
Sequential samples of single precipitation event were collected by the use of specially de-signed semi-automatic sequential precipitation collector in the spring of 1988 in Guilin City. ThePH value and soluble chemica...Sequential samples of single precipitation event were collected by the use of specially de-signed semi-automatic sequential precipitation collector in the spring of 1988 in Guilin City. ThePH value and soluble chemical species such as SO, NO, NH, Ca￣(2+), Mg￣(2+), Na￣+, K`+, F￣- andCl￣- were analyzed. An apparent decrease in the concentration of all ions except H￣+ and NO wasobserved at the initial portion of the events. The relative acidity increased as the event progress.The concentration of H￣+ was the result of comprehensive actions of all ions. The average scavengingratio of events was calculated and it is found that SO was the major contributor for acid rain inGuilin and Ca￣(2+) was the important neutralizer.展开更多
利用北京地区5 min间隔的自动气象站降水观测资料,SA雷达观测资料、FY-2卫星TBB(Temperature of Black Body)资料、常规气象探空资料和1°×1°NCEP/NCAR最终分析资料,对2006—2013年发生的10次极端暴雨事件(14个区(县)中,...利用北京地区5 min间隔的自动气象站降水观测资料,SA雷达观测资料、FY-2卫星TBB(Temperature of Black Body)资料、常规气象探空资料和1°×1°NCEP/NCAR最终分析资料,对2006—2013年发生的10次极端暴雨事件(14个区(县)中,任意一个区县代表站24 h内降水量≥100 mm,且暴雨区内至少有一个自动气象站降水强度≥40 mm/h)的基本特征进行了对比分析。结果表明:(1)长生命周期的单体或多单体组织合并的中尺度对流系统(第Ⅰ类中尺度对流系统)形成的暴雨中心一般位于北京西部山前地区或中心城区,这种分布与低空偏东气流的地形强迫作用或城市强迫作用有关;"列车效应"对应的多单体中尺度对流系统(第Ⅱ类中尺度对流系统)形成的极端暴雨事件往往与两次不同属性的降水过程有关:锋前暖区对流过程和锋面附近的对流过程。因此,降水分布往往平行于低空急流轴或锋面。(2)第Ⅰ类中尺度对流系统形成的极端暴雨过程局地性更强,全市平均降水量远小于暴雨量级(50 mm),其中,由混合型降水主导的极端暴雨事件一般是由几乎不移动的长生命周期单体反复生消造成的,对流高度相对较低;而深对流主导的极端暴雨事件一般由多单体组织、合并、加强造成,由于对流单体的上冲云顶很高,最低TBB一般低于-55℃,这类极端暴雨事件的短时强降水具有显著的间歇性:第一阶段的强降水与单体对流发展过程对应,以后的短时强降水与对流单体组织、合并过程对应。(3)"列车效应"对应的多单体中尺度对流系统暴雨过程,初始阶段一般表现为相互独立的两个对流带,即与锋面系统对应的对流带和与低空急流轴对应的暖区对流带,随着锋面对流带逐渐向暖区对流带移动,低空冷空气逐渐侵入到暖区对流带中,两条对流云带逐渐合并,对流活动进一步发展;或者由于暖区对流带截断锋面对流带的水汽入流,造成�展开更多
文摘根据作者提出的 Ca CO3淀积深度理论、风化剖面的野外鉴别和室内 Ca CO3、磁化率测定、粒度分析 ,确定了陕西长武第 4、第5层古土壤底部之下存在深部风化黄土层和迁出了土壤层的 Ca CO3结核层。这种风化黄土层和 Ca CO3淀积层的发育表明当时风化淋滤作用超出了成壤带深度范围 ,指示长武第 4、第 5层古土壤为不具 Ca CO3淀积层的中酸性、淋溶型森林土壤。该风化层代表了降水丰富的气候事件 ,当时年均降水量为 90 0 mm左右。
基金supported by the National Natural Science Foundation of China (31171506 and 31071375)
文摘To accurately evaluate the carbon sequestration potential and better elucidate the relationship between the carbon cycle and regional climate change, using eddy covariance system, we conducted a long-term measurement of CO 2 fluxes in the rain-fed winter wheat field of the Chinese Loess Plateau. The results showed that the annual net ecosystem CO 2 exchange （NEE） was （-71.6±5.7） and （-65.3±5.3） g C m-2 y-1 for 2008-2009 and 2009-2010 crop years, respectively, suggesting that the agro-ecosystem was a carbon sink （117.4-126.2 g C m-2 yr-1）. However, after considering the harvested grain, the agro- ecosystem turned into a moderate carbon source. The variations in NEE and ecosystem respiration （R eco ） were sensitive to changes in soil water content （SWC）. When SWC ranged form 0.15 to 0.21 m3 m-3, we found a highly significant relationship between NEE and photosynthetically active radiation （PAR）, and a highly significant relationship between R eco and soil temperature （T s ）. However, the highly significant relationships were not observed when SWC was outside the range of 0.15-0.21 m3 m-3. Further, in spring, the R eco instantly responded to a rapid increase in SWC after effective rainfall events, which could induce 2 to 4-fold increase in daily R eco , whereas the R eco was also inhibited by heavy summer rainfall when soils were saturated. Accumulated R eco in summer fallow period decreased carbon fixed in growing season by 16- 25%, indicating that the period imposed negative impacts on annual carbon sequestration.
文摘利用南京大学浦口校区大气科学园的近地层湍流脉动资料及Meteorological InformationComprehensive Analysis and Process System气象数据资料,针对2008年5月南京地区一次降水过程,分析比较了降水前后的湍流强度、归一化湍流动能、近地层通量输送和速度能谱特征.结果表明:从气象要素上看,降水临近时风速变化大,温度、气压降低明显,降水期间湿度很高.从湍流特征上看,降水时湍流强度突变增大,归一化湍流动能也变大,湍流活动增强;u、v方向动量输送-u′w′、-v′w′强度都增大,但输送方向相反,此时近地层归一化摩擦速度也明显变大;感热通量w′T′迅速减小,甚至微弱逆向输送;降水前后风速能谱惯性副区基本满足Kolmogorov的-2/3次方律,降水时u、v能谱低频段峰值频率左移明显,分析低频段峰值对应涡的尺度发现,近地层中降水前后贡献湍流能量最大的涡尺度存在很大差异.
文摘Quantitative precipitation estimation and rainfall monitoring based on meteorological data, potentially provides continuous, high-resolution and large-coverage data, are of high practical use: Think of hydrogeological risk management, hydroelectric power, road and tourism. Both conventional long-range radars and rain-gauges suffer from measurement errors and difficulties in precipitation estimation. For efficient monitoring operation of localized rain events of limited extension and of small basins of interest, an unrealistic extremely dense rain gauge network should be needed. Alternatively C-band or S-band meteorological long range radars are able to monitor rain fields over wide areas, however with not enough space and time resolution, and with high purchase and maintenance costs. Short-range X-band radars for rain monitoring can be a valid compromise solution between the two more common rain measurement and observation instruments. Lots of scientific efforts have already focused on radar-gauge adjustment and quantitative precipitation estimation in order to improve the radar measurement techniques. After some considerations about long range radars and gauge network, this paper presents instead some examples of how X-band mini radars can be very useful for the observation of rainfall events and how they can integrate and supplement long range radars and rain gauge networks. Three case studies are presented: A very localized and intense event, a rainfall event with high temporal and spatial variability and the employ of X-band mini radar in a mountainous region with narrow valleys. The adaptability of such radar devoted to monitor rain is demonstrated.
文摘The detailed analysis of individual rain events characteristics is an essential step for improving our understanding of variation in precipitation over different topographies. In this study, the homogeneity among rain gauges was investigated using the concept of “rain event properties,” linking them to the main atmospheric system that affects the rainfall in the region. For this, eight properties of more than 23,000 rain events recorded at 47 meteorological stations in Mumbai, India, were analyzed utilizing seasonal (June-September) rainfall records over 2006-2016. The high similarities among the properties indicated the similarities among the rain gauges. Furthermore, similar rain gauges were distinguished, investigated and characterized by cluster analysis using self-organizing maps (SOM). The cluster analysis results show six clusters of similarly behaving rain gauges, where each cluster addresses one isolated class of variables for the rain gauge. Additionally, the clusters confirm the spatial variation of rainfall caused by the complex topography of Mumbai, comprising the flatland near the Arabian Sea, high-rise buildings (urban area) and mountain and hills areas (Sanjay Gandhi National Park located in the northern part of Mumbai).
文摘Sequential samples of single precipitation event were collected by the use of specially de-signed semi-automatic sequential precipitation collector in the spring of 1988 in Guilin City. ThePH value and soluble chemical species such as SO, NO, NH, Ca￣(2+), Mg￣(2+), Na￣+, K`+, F￣- andCl￣- were analyzed. An apparent decrease in the concentration of all ions except H￣+ and NO wasobserved at the initial portion of the events. The relative acidity increased as the event progress.The concentration of H￣+ was the result of comprehensive actions of all ions. The average scavengingratio of events was calculated and it is found that SO was the major contributor for acid rain inGuilin and Ca￣(2+) was the important neutralizer.
文摘利用北京地区5 min间隔的自动气象站降水观测资料,SA雷达观测资料、FY-2卫星TBB(Temperature of Black Body)资料、常规气象探空资料和1°×1°NCEP/NCAR最终分析资料,对2006—2013年发生的10次极端暴雨事件(14个区(县)中,任意一个区县代表站24 h内降水量≥100 mm,且暴雨区内至少有一个自动气象站降水强度≥40 mm/h)的基本特征进行了对比分析。结果表明:(1)长生命周期的单体或多单体组织合并的中尺度对流系统(第Ⅰ类中尺度对流系统)形成的暴雨中心一般位于北京西部山前地区或中心城区,这种分布与低空偏东气流的地形强迫作用或城市强迫作用有关;"列车效应"对应的多单体中尺度对流系统(第Ⅱ类中尺度对流系统)形成的极端暴雨事件往往与两次不同属性的降水过程有关:锋前暖区对流过程和锋面附近的对流过程。因此,降水分布往往平行于低空急流轴或锋面。(2)第Ⅰ类中尺度对流系统形成的极端暴雨过程局地性更强,全市平均降水量远小于暴雨量级(50 mm),其中,由混合型降水主导的极端暴雨事件一般是由几乎不移动的长生命周期单体反复生消造成的,对流高度相对较低;而深对流主导的极端暴雨事件一般由多单体组织、合并、加强造成,由于对流单体的上冲云顶很高,最低TBB一般低于-55℃,这类极端暴雨事件的短时强降水具有显著的间歇性:第一阶段的强降水与单体对流发展过程对应,以后的短时强降水与对流单体组织、合并过程对应。(3)"列车效应"对应的多单体中尺度对流系统暴雨过程,初始阶段一般表现为相互独立的两个对流带,即与锋面系统对应的对流带和与低空急流轴对应的暖区对流带,随着锋面对流带逐渐向暖区对流带移动,低空冷空气逐渐侵入到暖区对流带中,两条对流云带逐渐合并,对流活动进一步发展;或者由于暖区对流带截断锋面对流带的水汽入流,造成�
