探测大气温湿廓线的35通道微波辐射计设计原理与特点     

卢建平  黄建平  郭学良  于子平  雷连发  张北斗 《气象科技》2014,42(2):193-197

总结了自主研制的MWP967KV型地基35通道微波辐射计系统设计原理和主要特点。系统将K、V双频段宽带天线及接收机、宽带调谐本振、温湿压计以及电源模块紧凑集成为一台整机设备。对各传感器的测量输出实时进行一体化综合处理,采用BP神经网络实时反演大气温度、湿度廓线和汽、水总量。廓线的垂直覆盖范围为地表至顶空10km,共划分为58层。辐射计样机于2012年秋冬季节在北京地区开展了为期2个月的观测试验,利用这段时期内的69个探空资料样本对辐射计2个层次的实时观测输出都进行了对比检验,计算了水汽、氧气通道亮温和反演所得大气温湿廓线的平均偏差、均方差以及相关性。结果表明该系统能够满足实时气象监测的需求,达到国际先进水平。  相似文献   

The seasonal foot printing mechanism of spring Arctic sea ice in the Bergen climate models     

GUO Dong  GAO Yongqi  GONG Daoyi 《极地研究(英文版)》2014,(4)

The influence of spring Arctic sea ice variability on the Pacific Decadal Oscillation(PDO) like sea surface temperature(SST) variability is established and investigated using an Atmosphere Ocean General Circulation Model(AOGCM) of the Bergen Climate Model version 2(BCM2). The spring Arctic sea ice variability affects the mid-latitudes and tropics through the propagation of the anomalous Eliassen-Palm(E-P) flux from the polar region to mid- and low-latitudes during boreal spring. The pathway includes anomalous upward wave activity, which propagates to the high troposphere from near the surface of the polar region, turns southward between 500 h Pa and 200 h Pa and extends downward between 50°N and 70°N, influencing the near surface atmospheric circulation. The alteration of the near surface atmospheric circulation then causes anomalous surface ocean circulation. These circulation changes consequently leads to the SST anomalies in the North Pacific which may persist until the following summer, named seasonal "foot printing" mechanism(SFPM).  相似文献   

The Relationship between the East Asian Subtropical Westerly Jet and Summer Precipitation over East Asia as Simulated by the IAP AGCM4.0          下载免费PDF全文

YAN Zheng-Bin  LIN Zhao-Hui  ZHANG He 《大气和海洋科学快报》2014,7(6):487-492

Based on a 30-year Atmospheric Model Intercomparison Project（AMIP） simulation using IAP AGCM4.0, the relationship between the East Asian subtropical westerly jet（EASWJ） and summer precipitation over East Asia has been investigated, and compared with observation. It was found the meridional displacement of the EASWJ has a closer relationship with the precipitation over East Asia both from model simulation and observation, with an anomalous southward shift of EASWJ being conducive to rainfall over the Yangtze-Huaihe River Valley（YHRV）, and an anomalous northward shift resulting in less rainfall over the YHRV. However, the simulated precipitation anomalies were found to be weaker than observed from the composite analysis, and this would be related to the weakly reproduced mid-upper-level convergence in the mid-high latitudes and ascending motion in the lower latitudes.  相似文献   

Application of a Coupled Land Surface-Hydrological Model to Flood Simulation in the Huaihe River Basin of China   总被引：1，自引：0，他引：1       下载免费PDF全文

LI Min  LIN Zhao-Hui  YANG Chuan-Guo  SHAO Quan-Xi 《大气和海洋科学快报》2014,7(6):493-498

A hydrological simulation in the Huaihe River Basin（HRB） was investigated using two different models： a coupled land surface hydrological model（CLHMS）, and a large-scale hydrological model（LSX-HMS）. The NCEP-NCAR reanalysis dataset and observed precipitation data were used as meteorological inputs. The simulation results from both models were compared in terms of flood processes forecasting during high flow periods in the summers of 2003 and 2007, and partial high flow periods in 2000. The comparison results showed that the simulated streamflow by CLHMS model agreed well with the observations with Nash-Sutcliffe coefficients larger than 0.76, in both periods of 2000 at Lutaizi and Bengbu stations in the HRB, while the skill of the LSX-HMS model was relatively poor. The simulation results for the high flow periods in 2003 and 2007 suggested that the CLHMS model can simulate both the peak time and intensity of the hydrological processes, while the LSX-HMS model provides a delayed flood peak. These results demonstrated the importance of considering the coupling between the land surface and hydrological module in achieving better predictions for hydrological processes, and CLHMS was proven to be a promising model for future applications in flood simulation and forecasting.  相似文献   

Preliminary Assessment of the Common Land Model Coupled with the IAP Dynamic Global Vegetation Model          下载免费PDF全文

ZHU Jia-Wen  ZENG Xiao-Dong  LI Fang  SONG Xiang 《大气和海洋科学快报》2014,7(6):505-509

The Common Land Model（CoLM） was coupled with the IAP Dynamic Global Vegetation Model（IAPDGVM）, and the performance of this combined CoLMIAP model was evaluated. Offline simulations using both the original Common Land Model（CoLM-LPJ） and CoLM-IAP were conducted. The CoLM-IAP coupled model showed a significant improvement over CoLMLPJ, as the deciduous tree distribution decreased over temperate and boreal regions, while the distribution of evergreen trees increased over the tropics. Some biases in CoLM-LPJ were preserved, including the overestimation of evergreen trees in tropical savanna, the underestimation of boreal evergreen trees, and the absence of boreal shrubs. However, most of these biases did not exist in a further coupled simulation of IAP-DGVM with the Community Land Model（CLM）, for which the parameters of IAP-DGVM were optimized. This implies that further improvement is needed to deal with the differences between CoLM and CLM in parameterizations of landbased physical and biochemical processes.  相似文献   

Stationary Wave Activity Associated with the East Asian Winter Monsoon Pathway简          下载免费PDF全文

WANG Lin 《大气和海洋科学快报》2014,(1):7-10

The pathway of the East Asian winter monsoon（EAWM） that usually leads to the out-of-phase pattern of surface air temperature between northern and southern East Asia is an important feature in the variability of the EAWM besides its strength.Using the European Centre for Medium-Range Weather Forecasts 40-year（ERA40） reanalysis dataset,this study investigates the pathway-related stationary wave activity to explore the mechanism of the interannual variations in the EAWM pathway.It reveals that when the southern pathway of the EAWM is strong,the phase of the climatological stationary wave tends to be shifted westward significantly in both the horizontal and vertical directions by an anomalous wavenumber 2 pattern at mid-latitudes,whereas the changes are relatively small in the subtropics.The horizontal changes in the stationary wave phase facilitate a north-south-oriented East Asian trough in the middle troposphere that eventually produces the strong southern pathway of the EAWM.The vertical changes in the stationary wave,in contrast,feature a westward-tilted phase line with height over the North Pacific,indicating enhanced upward propagation of waves into the stratosphere.This result suggests that the phase of stationary waves at mid-latitudes dominate the interannual variations in the EAWM pathway.Moreover,it supports our previous interpretation of the possible role of the North Pacific sea surface temperature（SST） in the EAWM pathway variability.It also implies that the excitation of anomalous mid-latitude stationary waves may be the key in the response of the EAWM pathway to the North Pacific SST.  相似文献   

Real-Time Observation on Water-Soluble Ions of PM2.5in Beijing under the Influences of Different Air Masses in Summer简          下载免费PDF全文

CHENG Meng-Tian  SUN Yang  ZHU Xiao-Wan  CHAO Na 《大气和海洋科学快报》2014,(1):23-27

To further understand the variations of water-soluble ions in PM2.5 in Beijing,the authors observed their concentrations continuously and in high temporal resolution by the system for rapid collection of fine particles and ion chromatography（RCFP-IC） during 12–18 July 2010.These results combined with those of earlier backward trajectory research are used analyzed to determine the causes of concentration changes in water-soluble ions under the influences of two kinds of air masses in summer.The results indicate that concentrations of NO3^-,SO4^2-,and NH4＋ were influenced strongly by the continental air mass than by the marine air mass.Cl^- and Na^＋ were not changed significantly.Because the sources of K^＋,Mg^2＋,and Ca^2＋ are mainly concentrated on land,their concentration levels were slightly higher under the control of continental air mass than that of the marine air mass.Variations of NO2^- during the observation differed from those of other ions;its concentration was significantly higher under the influence of marine air mass.Moreover,the authors obtain the diurnal variations of eight water-soluble inorganic ions including NH4^＋,K^＋,Mg^2＋,Ca^2＋,Cl^-,NO2^-,NO3^-,and SO4^2-.Diurnal variations of NH4^＋,NO3^-,and Cl^- showed single peak,which appeared before noon,while SO4^2- showed two peaks that appeared during rush hours.Those of Mg^2＋,Ca^2＋,and K＋ showed single peak that appeared in the afternoon.That of NO2^- showed with a peak appearing at sunrise and a valley appearing at sunset.  相似文献   

Influence of Mass and Radius of Ice Crystals on Hydrometeors,Internal Energy,and Kinetic Energy: A Numeric Model Study简          下载免费PDF全文

RAN Ling-Kun  QI Yan-Bin  LI Na 《大气和海洋科学快报》2014,(1):49-55

Two cloud-scale experiments with two different ice-phase schemes were carried out for a precipitation event that occurred in eastern China in 2005.The results were analyzed to examine the influences of the change of ice-particle mass and radius on hydrometeors,internal energy,and kinetic energy,as well as the primary factors responsible.It was found that the ice content increases notably and the snow content decreases due to the change.This is the consequence of the modulation of cloud microphysical processes.In particular,the Bergeron process and the accretion of snow and cloud ice are markedly influenced.The differences of internal energy and kinetic energy between the two experiments are caused by adjustments to pressure-flux divergence,the coupling of temperature and divergence,and gravitational work,and the reason is that these three factors result in differences of local changes of internal and kinetic energy.  相似文献   

An Optical Disdrometer for Measuring Present Weather Parameters          下载免费PDF全文

JIA Sheng-Jie  Lü Da-Ren  XUAN Yue-Jian 《大气和海洋科学快报》2014,7(6):559-563

A new present weather identifier（PWI） based on occlusion and scattering techniques is presented in the study. The present weather parameters are detectable by the meteorological optical range（MOR） approximately up to 50 km and by droplets with diameters ranging from 0.125 mm to 22 mm with velocities up to 16 m s-1. The MOR error is less than 8% for the MOR within 10 km and less than 15% for farther distances. Moreover, the size errors derived from various positions of the light sheet by the particles were checked within ± 0.1 mm ± 5%. The comparison shows that the MOR, in a sudden shower event, is surprisingly consistent with those of the sentry visibility sensors（SVS） with a correlation coefficient up to 98%. For the rain amounts derived from the size and velocity of the droplets, the daily sums by the PWI agree within 10% of those by the Total Rain Weighing Sensor（TRwS205） and the rain gauge. Combined with other sensors such as temperature, humidity, and wind, the PWI can serve as a present weather sensor to distinguish several weather types such as fog, haze, mist, rain, hail, and drizzle.  相似文献   

大气初始场对短期气候数值预测的影响          下载免费PDF全文

官元红  周广庆  陆其峰  陆维松 《大气科学学报》2014,37(5):631-641

利用中国科学院大气物理研究所发展的九层大气环流模式(简称IAP 9L2°×2.5°-AGCM)分析了大气初始场对短期气候数值预测的影响,分别从实际观测海温、海冰的外强迫和气候态海温、海冰的外强迫出发,进行两组集合回报试验,每组包含3个试验,分别将实时NCEP-Ⅱ资料和对NCEP-Ⅱ资料经5 d平滑、11 d平滑后的资料作为大气初始场,进行17 a(1988—2004年)集合回报试验,采用相关分析方法对试验结果进行对比分析。结果表明,比较相关系数定量检验出大气初始场对热带地区可预报性影响较小,而对中、高纬度地区影响很大。通过对6个试验中对应气象要素在对流层各层距平时间相关系数以及17 a空间异常相关系数均值比较分析发现对东亚(中国)地区夏季气候而言,NCEP-Ⅱ资料经5 d平滑后生成的大气初始场对应回报试验结果相对最好。  相似文献