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971.
972.
Wave-dependence of friction velocity,roughness length,and drag coefficient over coastal and open water surfaces by using three databases 总被引:3,自引:0,他引:3
The parameterization of friction velocity, roughness length, and the drag coefficient over coastal
zones and open water surfaces enables us to better understand the physical processes of air-water interaction.
In context of measurements from the Humidity Exchange over the Sea Main Experiment (HEXMAX), we recently proposed
wave-parameter dependent approaches to sea surface friction velocity and the aerodynamic roughness by using the
dimensional analysis method. To extend the application of these approaches to a range of natural surface conditions,
the present study is to assess this approach by using both coastal shallow (RASEX) and open water surface measurements
(Lake Ontario and Grand Banks ERS-1 SAR) where wind speeds were greater than 6.44 m s-1. Friction velocities,
the surface aerodynamic roughness, and the neutral drag coefficient estimated by these approaches under moderate wind
conditions were compared with the measurements mentioned above. Results showed that the coefficients in these approaches
for coastal shallow water surface differ from those for open water surfaces, and that the aerodynamic roughness length
in terms of wave age or significant wave height should be treated differently for coastal shallow and open water surfaces. 相似文献
973.
974.
A nested-model system is constructed by embedding the regional climate model RegCM3 into a
general circulation model for monthly-scale regional climate forecast over East China. The systematic
errors are formulated for the region on the basis of 10-yr (1991-2000) results of the nested-model system,
and of the datasets of the Climate Prediction Center (CPC) Merged Analysis of Precipitation (CMAP) and
the temperature analysis of the National Meteorological Center (NMC), U.S.A., which are then used for
correcting the original forecast by the system for the period 2001-2005. After the assessment of the original
and corrected forecasts for monthly precipitation and surface air temperature, it is found that the corrected
forecast is apparently better than the original, suggesting that the approach can be applied for improving
monthly-scale regional climate dynamical forecast. 相似文献
975.
With the development of numerical weather prediction technology,the traditional global hydrostatic models used in many countries of the world for operational weather forecasting and numerical simulations of general circulation have become more and more unfit for high-impact weather prediction.To address this,it is important to invest in the development of global nonhydrostatic models.Few existing nonhydrostatic global models use consistently the grid finite difference scheme for the primitive equations of dynamical cores,which can subsequently degrade the accuracy of the calculations.A new nonhydrostatic global spectral model,which utilizes the Eulerian spectral method,is developed here from NCAR Community Atmosphere Model 3.0(CAM3.0).Using Janjic's hydrostatic/nonhydrostatic method,a global nonhydrostatic spectral method for the primitive equations has been formulated and developed.In order to retain the integrity of the nonhydrostatic equations,the atmospheric curvature correction and eccentricity correction are considered. In this paper,the Held-Suarez idealized test and an idealized baroclinic wave test are first carried out,which shows that the nonhydrostatic global spectral model has similar climate states to the results of many other global models for long-term idealized integration,as well as better simulation ability for short-term idealized integration.Then,a real case experiment is conducted using the new dynamical core with the full physical parameterizations of subgrid-scale physical processes.The 10-day numerical integration indicates a decrease in systematic error and a better simulation of zonal wind,temperature,and 500-hPa height. 相似文献
976.
The relationship between dust weather frequency (DWF), which denotes the
number of days of dust weather events, over Beijing and the East Asian
Monsoon (EAM) was studied using DWF data for Beijing during the period
1951--2006. Results show that, during this period, the blowing-dust weather
frequency (BDWF), as well as the indices of East Asian winter monsoon (EAWM)
and East Asian summer monsoon (EASM), all decreased considerably, with a
t-test confidence level of 99%. The correlation coefficients between the
chosen EAWM index and BDWF over Beijing in winter and the following spring
were 0.34 and 0.33, respectively, with significance levels of 0.01 and 0.02,
respectively. For the chosen EASM index and BDWF, these correlation
coefficients were 0.51 and 0.45, respectively, with both at a confidence
level exceeding 99.9%. With the linear trends removed, the values (in the
same order as above) were 0.14, 0.14, -0.12, and -0.09, all not significant
at the 95% confidence level. Clearly, the EAM relates mainly to DWF over
long timescales. To a certain extent, the EAM might have some impact on DWF
by affecting the associated surface air temperature and precipitation during
the corresponding time period in sand-dust source regions at the interannual
scale. A stronger (weaker) EAWM might advance (suppress) the occurrence of
DWF, and the opposite for the EASM. 相似文献
977.
利用全国660个常规气象站40年(1961-2000年)整编气象资料.采用逆距离权重反比法、样条函数法和普通克立格法等常用的3种插值方法,分析了直接插值法和综合余项法对气温插值的影响,提出了去除气温形成中的确定性部分后,以随机项进行插值可提高气温插值精度。并从空间上、时间上对比眲不同插值方法的误差,最后分析了气象站的空间分布密度对插值方法的敏感性。验证结果表明:除个别月份外,综合余项法的各项平均绝对误差均在1℃以内,比直接插值法减小了0.6~1.6℃,精度提高了38%~85%;且综合余项法的精度不依赖于台站密度的大小、插值方法的不同,具有较高的精确性和稳定性,这说明影响空间插值精度的关键因子并非是气象观测站点密度的提高、空问插值方法的改进。 相似文献
978.
“珍珠”(0601)异常急翘路径和内核结构变化的诊断分析及数值研究 总被引:4,自引:0,他引:4
使用FY2卫星TBB资料、NCEP最终分析资料(1°×1°)和中尺度模式WRF,对0601号强台风"珍珠"的"急翘"异常转向路径和内核结构变化进行诊断分析和数值模拟。结果表明:"珍珠"移向变化与环境引导气流和位涡倾向1波分量正异常有关,"急翘"前12小时,环境引导气流向北偏转,位涡倾向1波分量正异常对应着"珍珠"移动方向变化;内核非对称结构发展与环境风垂直切变演变有关,垂直切变使得涡旋倾斜,涡旋倾斜方向出现较强的上升运动,导致"珍珠"内核偏南象限对流活动较强。 相似文献
979.
由850hPa的风场资料和海平面气压资料计算两个东亚冬季风强度指数,结合月平均降水资料,分析我国南方冬季降水对冬季风响应的空间分布型及其在冬季各月的差异。结果表明:12月东亚冬季风强度比1、2月的弱,同期的降水对其响应不明显;1月冬季风比2月强,同期降水对季风的响应比2月更强些。在1、2月,强(弱)东亚冬季风易造成南方冬季降水偏少(多),但这种响应是时间和空间的函数,随时间变化且有明显的区域特征。1月的强响应区基本上连成一片,强响应中心散布于其中;最明显的中心区在淮河以南附近,区域中心值-0.5;响应强度由此中心向南变弱,但依然分别在湖南东北部、江西东北部以及四川东北部都出现了较强中心区,区域中心值都为-0.35左右;2月的响应区相对1月作了总体的顺时针偏转和稍微的北缩。分析发现,响应区的空间分布可以从地形和地势分布解释,响应区的时间变化与850hPa的风场有关。 相似文献
980.
采用CAM3(Community Atmosphere Model Version3)模式中海气湍流通量参数化原方案和改进方案,利用观测海温驱动CAM3模式进行气候模拟,以分析模式对厄尔尼诺事件影响气候变化的模拟能力。结果表明,采用CAM3模式海气湍流通量参数化改进方案,模式能够更好地模拟出由厄尔尼诺事件引起的北太平洋和北美地区大气环流的变化,尤其是对厄尔尼诺年冬季阿留申低压强度和与PNA遥相关型有关的500hPa位势高度异常的模拟。 相似文献