甚低纬多跳哨声的非导管传播

实验发现,在磁纬20°以下区域地面可重复接收到多跳哨声.本文着重考察了低纬多跳哨声非导管传播的可能性.计算结果证明,在给定的电离层状态下,该地区可以形成多跳哨声的非导管传播路径.射线追踪得到的多跳路径特征能满意地解释文中所列实验结果.因此,作为一种可能的传播机制,低纬多跳哨声的非导管传播方式值得重视.     

甚低纬多跳哨声的非导管传播

实验发现,在磁纬20°以下区域地面可重复接收到多跳哨声.本文着重考察了低纬多跳哨声非导管传播的可能性.计算结果证明,在给定的电离层状态下,该地区可以形成多跳哨声的非导管传播路径.射线追踪得到的多跳路径特征能满意地解释文中所列实验结果.因此,作为一种可能的传播机制,低纬多跳哨声的非导管传播方式值得重视.     

The Impact of Arctic Ozone Depletion on Northern Middle Latitudes: Interannual Variability and Dynamical Control

We have investigated the effect of the export of Arctic ozone loss, or`dilution', on mid-latitude ozone depletion during the 1990s, and its relation tointerannual meteorological variability. A stratospheric chemical-transport modelincorporated a simple gas-phase ozone scheme with the addition of a parameterisation ofpolar depletion which depended only on temperature and duration of sunlight. Themodel was forced with the U.K. Meteorological Office analyses from 1991 to 1999 covering eight Northern Hemisphere winters. The modelled Arctic ozone column losses wereabout half the magnitude of those in the Antarctic and showed a considerablevariation from year to year. The northern middle latitudes (40°–60° N)were mainly affected through dilution and experienced a variable 5–20%depletion. Year-round there is a depletion of about 1% in northern middle latitudes due toactivation at the pole but there is no evidence that this depletion increases with timeduring this integration. A series of inert tracer experiments for the winters from 1996 to 1999 showed that the dilution occurs primarily at the 560 K and 465 K isentropic levels where up to 30% of the airoriginating northward of 67° N on 1 March is found at 47° N later in spring. Thestrength and persistence of the Arctic vortex were crucial in determining the severity and the timing of the ozone dilution every year by influencing, respectively, the magnitude of the high-latitude depletion and the effectiveness of mixing to lower latitudes. This spring dilution was correlated with the winter/spring planetary wave activity indicating the important role of dynamical processes in regulating the polar-driven mid-latitude ozone depletion.     

地磁场Sq的经度效应和UT变化

使用国际地球物理年（ＩＧＹ）和国际地球物理合作年（ＩＧＣ）期间全球地磁台网的资料和中国台站的同期地磁记录，对地磁场太阳日变化Ｓ_ｑ的经度效应和ＵＴ变化进行了分析研究．将适用于瞬时全球磁场的球谐分析法与适用于平均场的双调和分析法相结合，提出了一种分析Ｓ_ｑ磁场的新方案，得到了（θ，Ｔ，ｔ）坐标系中组成Ｓ_ｑ场的三个部分，即仅随地方时ＬＴ变化的部分Ｓ_ＬＴ，仅随世界时ＵＴ变化的部分Ｓ_ＵＴ以及既随ＬＴ变化又随ＵＴ变化的部分Ｓ_ＬＵＴ．从全球来看，在ＩＧＹ／ＩＧＣ期间，这三部分的强度之比分别为：Ｘ分量１．０：０．２：０．３，ｙ分量１．０：０．１：０．６，Ｚ分量１．０：０．４：１．０．Ｓ_ｑ的经度效应和ＵＴ变化虽然表现了同一物理过程，但它们有不同的表达形式，其决定因素是地磁轴对地理轴的倾斜，地磁场的非偶极子成分（即区域性异常）和地球内部电性的横向不均匀性（包括海陆分布、地壳上地幔电导率的区域差异）     

On geophysical explanation of some irregular variations of the mean latitudes of latitude stations

Mean latitude variations computed by Orlovs or other filters have some irregular variations in addition to secular ones. These are of the order of ±0.05 to ±0.1, they can last several years and sometimes show regional similarities. In looking for an explanation of such latitude variations several physical mechanisms have been investigated. The most probable one is the mechanism of stress propagation in the lithosphere and asthenosphere. The consequent gravitational and deformational effects could explain both the magnitude and the time dependance of the irregular latitude variations.     

2017年秋季河南罕见连阴雨天气特征及成因分析

2017年8月下旬至10月中旬河南发生了近14a来罕见秋季连阴雨过程。利用1961—2017年河南省地面气候整编资料和NCEP/NCAR再分析资料,采用相关分析法、T检验、小波分析及带通滤波等方法,对此次连阴雨过程的大气环流特点进行分析。结果表明:2017年秋季河南连阴雨期间,乌拉尔山高压脊、贝加尔湖低槽和西太平洋副热带高压较常年同期偏强且长时间维持;东欧和里海—巴尔喀什湖两个地区是此次连阴雨过程的上游关键区域,东欧地区大气环流具有准双周到30d的振荡周期,里海—巴尔喀什湖地区具有4—8d的振荡周期。东亚200hPa急流轴东西跨度和急流核的极大风速较常年同期偏大;急流区西南部的辐散区在河南上空有抽吸作用,有利于降水的发生;高空急流纬向风速有三次加强过程,与三次连阴雨过程相对应。在不同的连阴雨阶段水汽输送源地和输送通道不同,三个阶段的水汽来源分别为印度洋、中国南海和西太平洋。     

Global snowmelt flood disasters and their impact from 1900 to 2020北大核心CSCD

Under the background of climate warming, the occurrence time, frequency, intensity, and impact of snowmelt flood disasters have changed significantly. Thus, establishing a global snowmelt flood disaster database is particularly important for disaster risk management. With the help of a web crawler, and based on multiple data sources such as natural disaster databases, documents, books, government agency websites, and news media, this study collected relevant information of snowmelt floods and mixed floods and established standards for identifying snowmelt flood events and their disaster impacts based on data from the different sources. Following the screening, sorting, fusion, and integration of snowmelt flood events, a global snowmelt flood disaster dataset containing 579 pieces of data with strong pertinence and reliability was constructed. The temporal and spatial distribution characteristics of global snowmelt flood disasters from 1900 to 2020 were preliminarily analyzed. The results showed that the snowmelt floods were mainly distributed between 30° N and 60° N, with more mixed floods south of 50° N and more snowmelt floods north of 50° N. Spring was the period of highest incidence of snowmelt flood disasters, followed by winter, summer, and autumn, respectively. The snowmelt floods that occurred in spring, autumn, and winter were mainly at 40°~50° N, and the snowmelt floods that occurred in summer were mainly at 30°~40° N. Compared with the snowmelt floods, the mixed floods were more frequent and more destructive, and their frequency increased with climate warming. The results provide a scientific basis for risk prevention and loss assessment of global snowmelt flood disasters. © 2022 Science Press (China).     

前期中高纬大气环流异常与我国汛期雨带类型关系的研究

使用国家气候中心提供的1951～2002年北半球500 hPa高度上的月平均格点资料,对前期(1～5月)中高纬大气环流的异常与中国汛期雨带类型分布的关系进行了研究.结果表明,冬季(1～2月)500hPa环流的时空演变与中国汛期雨带类型分布有明显的相关,春季(3～5月)是转换季节,与雨带类型分布的关系不如冬季密切.尽管不同的雨带类型对应不同的高度距平合成场,但各雨型的高度距平之间只存在三个显著性差异区,且各雨带类型的西风指数显著性差异区与同期高度距平合成场的显著性差异区的经度范围一致.1、2月第一与第二显著     

Measurements and Models of the Mass Balance of Hintereisferner

This paper summarizes the methods applied to determine the mass balance of Hintereisferner and several other glaciers in the Tyrolean Alps since 1952. On an annual basis the direct glaciological method was applied with fixed date measurements on 10–15 accumulation pits and 30–90 ablation stakes on 9 km².
Indirect mass balance determination from equilibrium line altitude, accumulation area ratios or representative stakes, yield fair results and some exceptions could be related to anomalous meteorological conditions.
Monthly or more frequent stake readings supplied time series of ablation at various altitudes and slope aspects that served as basis for the calibration of energy and mass balance models. Of various models developed, two are presented in this paper. Both are based on degree days, one using daily values from a valley station to predict the mean annual balance of the entire glacier, while the other calculates day-to-day changes at 50-m grid points on the glacier.
The geodetic method has been applied for longer periods and yields results consistent with those of the glaciological method. The balance velocity calculated from recent ice thickness soundings and accumulation measurements is significantly less than observed velocity.     

Mass Balance Measurements on the Lemon Creek Glacier, Juneau Icefield, Alaska 1953–1998

Annual balance measurements on the Lemon Creek Glacier, Alaska conducted by the Juneau Icefield Research Program (JIRP) from 1953 through 1998 provide a continuous 46 year record. This is one of the nine American glaciers selected in a global monitoring network during the International Geophysical year, 1957/58. These data have been acquired primarily by employing consistent ground methods, conducted on similar annual dates and calculated using comparable methodology. The results have been until now fairly precise, but of uncertain accuracy. An adjunct comparison of topographic surface maps of the glacier made in 1957 and 32 years later in 1989 provides a rough determination of glacier surface elevation changes which are clearly of less precision than the compilation of annual ground data. Airborne surface profiling in 1995, and global positioning system leveling transects in 1996–1998 update the record of surface elevation changes over the past decade. The mean glacier ice thickness reductions suggested by these methods from 1957–1989, from 1957–1995 and from 1957–1998 are ?13.2 m, ?16.4 m, and ?21.7 m, respectively. It is of interest that the geodetic interpretations agree fairly well with the trend of sequential balances from ground-level stratigraphic measurements. To date, however, the infrequent mapping methods in this study have yielded specific balances averaging between 5 and 11% less than those resulting from our annual on-site glaciological monitoring. For future studies this can be an important factor. The ground data are, therefore, the ones in which we have most confidence. These show cumulative ice losses of ?13.9 m (12.7 m water equivalent w.e.) from 1957–1989, of ?19.0 m (?17.1 m w.e.) from 1957–1995, of ?24.4 m (22 m w.e.) from 1957–1998, and ?24.7 m (22.2 m w.e.) for the total cumulative loss over the full 46 years between 1953 and 1998. Although the balance trend has been increasingly negative it averages ?0.48 m/a in w.e. or 0.52 m of ice loss per year. To refine the reliability of density determinations in this data set the effects of internal accumulation from refrozen meltwater producing diagenetic ice structures in the annual firnpack have been taken into account. An unusual dearth of such structures within the 1997/98 firnpack provided a unique opportunity to facilitate application of the probing technique over broad areas of the nv. This added to our ground truth and verified accuracy of the test-pit measurements used in these long-term mass balance computations. The glacier's continuing negative mass balance has fueled a terminal retreat of 800 m during the 1953–1998 period. The annual balance trend indicates that despite a higher mean elevation and a higher elevation terminus from thinning and retreat, mean annual balance has been strongly negative since 1977 (?0.78 m/a w.e.). Dramatically increased negative mass balances have occurred in the 1990s, with 1996 and 1997 being the only years on record with no retained accumulation since field observations were initiated in the glacier source areas in 1948.