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181.
Observations made with the co-located Rayleigh lidar and MST radar systems at Aberystwyth (52.4°N, 4.1°W) in Wales and radiosondes from Valentia (51.9°N, 10.2°W) in Eire are used to investigate the changes in the vertical propagation of gravity waves during periods of 4 days in June 1995 and February 1993. In each month, the lidar observations show that the wave activity in the upper stratosphere and lower mesosphere changes between two pairs of days. The radar and radiosonde measurements indicate that mountain waves make no contribution to the changes in intensity. Instead, the changes seem to arise largely from the presence or absence of long-period waves with vertical wavelengths near 8 and 10 km in June and February, respectively. The influence of such waves on the vertical wavenumber spectra is examined and related to the evidence for convective instabilities provided by the temperature profiles. 相似文献
182.
Relict Shorelines and Ice Flow Patterns of the Northern Puget Lowland From Lidar Data and Digital Terrain Modelling 总被引:1,自引:0,他引:1
Dori J. Kovanen Olav Slaymaker 《Geografiska Annaler: Series A, Physical Geography》2004,86(4):385-400
Airborne lidar data from the northern Puget Lowland provide information on the spatial variability and amplitude of raised postglacial shorelines, marine deltaic features and glaciomarine sediments deposited between approximately c. 12 920 and 11 050 14C yr BP (15 960‐12 364 cal yr BP). Relict shorelines preserved in embayments on Whidbey and Camano islands (between 47°54′N and 48°24′N) are found up to an altitude of c. 90 m and record glacio‐isostatic movements attributed to postglacial rebound. The tilt of the regional minimum highstand sea level surface to the north of 0.80 m km?1, with local variability from 0.25 m km?1 to 0.77 m km?1, is consistent with previous studies (Thorson 1989; Dethier et al. 1995). The local variability is related to the uncertainty in the depth of the water column above these features at the time of deposition and probable tectonic deformation. The information generated by these lidar data is most valuable in posing new research questions, generating alternative research hypotheses to those already formulated in the northern Puget Lowland. 相似文献
183.
胡顺星 naol.hfcas.ac.cn 胡欢陵 naol.hfcas.ac.cn 周军 naol.hfcas.ac.cn 吴永华 naol.hfcas.ac.cn 《Acta Meteorologica Sinica》2002,(2)
In this paper the effects of aerosol on tropospheric ozone measurements by three-wavelength(266-289-308nm) dual differential absorption lidar (DIAL) and two-wavelength (266-289 nmand 266-308 nm) DIAL are simulated.By using the two kinds of DIAL.vertical profiles of ozonedensity from 2 to 3.6 km altitude range are measured.Both simulation and observation resultsshow that the three-wavelength dual-DIAL method is more effective to reduce the effects of aerosolthan the two-wavelength DIAL method.Therefore,accurate ozone density distributions can beretrieved by the three wavelength dual DIAL method. 相似文献
184.
本文利用2016年12月至2017年11月期间晴朗少云天气下的成都微脉冲激光雷达观测数据反演的混合层高度,与温江探空资料确定的混合层高度进行了对比和误差分析,结果表明:基于探空资料和激光雷达数据反演的混合层高度具有较好的一致性,两者相关系数达0.75,激光雷达反演的混合层高度略低于基于探空资料确定的值,在混合层高度为1000~2000m时,两种方法计算所得的值偏差幅度最小,约为20%;在1000m以内和2000m以上,偏差幅度略有增大,为26%;两种方法反演的混合层高度变化趋势较为一致,均呈现出12月、1月较低,4月、5月较高的特点;混合层高度具有明显的日变化特征:上午混合层高度迅速增高,午后增长速度减慢并发展到最大高度,日落后迅速降低;混合层内相对湿度的增加、残留层的存在是导致激光雷达反演混合层高度时产生较大误差的原因之一。 相似文献
185.
介绍了合成孔径技术的发展及其基本原理,对国外合成孔径激光雷达的发展进行了综述,最后对合成孔径激光雷达的优势进行了分析. 相似文献
186.
A vertical sounding of severe haze process in Guangzhou area 总被引:1,自引:0,他引:1
We detected a severe haze process in Guangzhou area with lidar and microwave radiometer, performed an inversion to get boundary layer height by wavelet covariance transform, and analyzed the correlation between meteorological factors of boundary layer and visibility from the perspective of dynamical and thermodynamic structures. Our results indicate that the boundary layer height shows significant daily changes, consistent with ground visibility variation. During the cleaning process, the boundary layer height exceeded 1 km; during severe haze, the height was only 500 m. Temperature gradient of 50–100 m, which was 30 h lag, was remarkably correlated with visibility, with the correlation coefficient of 0.77. High layer visibility(255 m) and low layer stability were significantly anticorrelation, and the maximum anticorrelation coefficient was up to-0.76 in cleaning days and-0.49 in haze days. In the related boundary layer meteorological factors, surface ventilation coefficient was linearly correlated with ground visibility, with the greatest correlation coefficient of 0.88. The correlation coefficients of boundary layer height, ground wind velocity, relative humidity and ground visibility were 0.76, 0.67, and-0.77, respectively. There was a strong correlation between different meteorological factors. The dominant meteorological factor during this haze process was surface ventilation coefficient. In the area without boundary layer height sounding, ground visibility and wind velocity could be used to estimate boundary layer height. 相似文献
187.
Robert M. Banta 《Acta Geophysica》2008,56(1):58-87
This paper reviews results from two field studies of the nocturnal stable atmospheric boundary layer (SBL) over the Great
Plains of the United States. Data from a scanning remote-sensing system, a High-Resolution Doppler Lidar (HRDL), provided
measurements of mean and turbulent wind components at high spatial and temporal resolution through the lowest 500–1000 m of
the atmosphere. This data set has allowed the characteristics of the low-level jet (LLJ) maximum (speed, height, direction)
to be documented through entire nights. LLJs form after sunset and produce strong shear in the layer below the LLJ maximum
or nose, which is a source of turbulence and mixing in the SBL. Simultaneous HRDL measurements of turbulence quantities related
to turbulence kinetic energy (TKE) has allowed the turbulence in the subjet layer to be related to LLJ properties. Turbulence
structure was found to be a function of the bulk stability of the subjet layer. For the strong-LLJ (> 15 m s−1), weakly stable cases the strength of the turbulence is proportional to the strength of the LLJ. For these cases with nearly
continuous turbulence in the subjet layer, low-level jet scaling, in which lengths are scaled by the LLJ height and velocity
variables are scaled by the LLJ speed, was found to be appropriate. For the weak-wind (< 5 m s−1 in the lowest 200 m), very stable boundary layer (vSBL), the boundary layer was found to be very shallow (sometimes < 10
m deep), and turbulent fluxes between the earth’s surface and the atmosphere were found to be essentially shut down. For more
intermediate wind speeds and stabilities, the SBL shows varying degrees of intermittency due to various mechanisms, including
shearinstability and other gravity waves, density currents, and other mesoscale disturbances. 相似文献
188.
机载激光雷达技术是一种利用激光对地表三维坐标精确信息进行采集的新型遥感技术。本文以长江三峡工程库区滑坡灾害调查和监测应用为主要研究目标,通过对试验区的机载激光雷达数据的获取和处理,得到了精度很高的机载激光雷达DEM产品,并从定性和定量两个方面进行了机载激光雷达技术滑坡调查和动态监测应用试验。研究表明机载激光雷达山体阴影图能够直观表达微地貌形态;机载激光雷达坡度和地表粗糙度图像能够提供精确的微地貌特征量;利用多期机载激光雷达数据进行滑坡动态监测,可以掌握一定时间段内滑坡体的变形趋势和特征,并精确测算变形量。 相似文献
189.
190.