The Characteristics of Storm Wave Behavior and Its Effect on Cage Culture Using the ADCIRC+SWAN Model in Houshui Bay,China     

Chao Yin  Haijun Huang  Daoru Wang  Yanxia Liu  Ziyue Guo 《中国海洋大学学报(英文版)》2020,19(2):307-319

The current storm wave hazard assessment tends to rely on a statistical method using wave models and fewer historical data which do not consider the effects of tidal and storm surge.In this paper,the wave-current coupled model ADCIRC+SWAN was used to hindcast storm events in the last 30 years.We simulated storm wave on the basis of a large set of historical storms in the North-West Pacific Basin between 1985 and 2015 in Houshui Bay using the wave-current coupled model ADCIRC+SWAN to obtain the storm wave level maps.The results were used for the statistical analysis of the maximum significant wave heights in Houshui Bay and the behavior of wave associated with storm track.Comparisons made between observations and simulated results during typhoon Rammasun(2014)indicate agreement.In addition,results demonstrate that significant wave height in Houshui Bay is dominated by the storm wind velocity and the storm track.Two groups of synthetic storm tracks were designed to further investigate the worst case of typhoon scenarios.The storm wave analysis method developed for the Houshui Bay is significant in assisting government's decision-making in rational planning of deep sea net-cage culture.The method can be applied to other bays in the Hainan Island as well.  相似文献   

Provenance and Tectonic Implications of Paleozoic Strata in the South Yellow Sea Basin,China–Revealed from the Borehole CSDP-2     

Gao  Xiaohui  Zhang  Xunhua  Guo  Xingwei  Cai  Laixing  Hou  Fanghui  Zhu  Xiaoqing 《中国海洋大学学报(英文版)》2020,19(3):536-550

Well CSDP-2 is a fully coring deep drilling hole, penetrating the thick Paleozoic marine strata in the South Yellow Sea Basin(SYSB) in the lower Yangtze Block(LYB). Based on the petrological and geochemical analysis of 40 sandstone samples from the core CSDP-2, the provenance and tectonic features of Paleozoic detrital rocks from SYSB are analyzed and systematically delineated in this article. The results show that the Silurian – Carboniferous sandstones are mature sublitharenite, while the Permian sandstones are unstable feldspathic litharenite. The average CIA(chemical index of alteration) is 74.61, which reflects these sediments were derived from source rocks with moderate chemical weathering. The REE(rare earth element) patterns are characterized by LREE enrichment, flat HREE and obviously negative Eu anomaly, which are similar to that of the upper continental crust. Dickinson QFL discrimination results indicate the recycled orogeny provenance. Various diagrams for the discrimination of sedimentary provenance based on major and trace element data show all the sediments were derived predominantly from quartz sedimentary rocks, of which the Permian strata contain more felsic sedimentary rocks. Geochemical data for these detrital rocks suggest they occur at the passive continental margin and island arc settings, and the Permian sandstone presents active continental margin setting.  相似文献   

1979～2020年北极和青藏高原臭氧低值区的动力输送特征比较     

王启璐  徐雯雯  涂静怡  于淑洋  饶建  郭栋 《大气科学》2023,(3):866-880

基于ERA5月平均再分析资料,利用Lorenz环流分解方法从定常和瞬变以及基流和涡旋的角度对比了北极与青藏高原臭氧低值区的动力输送特征。结果表明：动力总输送在两地上平流层作用最强,均使其臭氧浓度降低,且定常输送均强于瞬变输送,纬向与经向输送的作用均大致相反。然而,动力输送在北极地区的作用强度远大于青藏高原地区。北极地区纬向输送使得平流层中上层臭氧浓度降低,平流层下层臭氧浓度升高,经向输送的作用与之相反且强度明显偏弱,二者均主要作用于上平流层。青藏高原地区纬向和经向输送除在上平流层均使得臭氧浓度降低外,二者作用大致相反且强度相当,输送大值区在垂直方向上存在双中心结构,分别位于上平流层与上对流层—下平流层（Upper Troposphere–Lower Stratosphere,简称UTLS）区。两地区纬向和经向输送的差异均主要由定常涡旋输送所造成。青藏高原地区定常与瞬变输送的强度差异没有北极地区大。此外,两地定常和瞬变输送中涡旋对臭氧纬向平均的输送均起到主要作用,体现出涡旋输送在两地臭氧浓度变化的动力输送过程中发挥着至关重要的作用。  相似文献   

Ambiguity resolved precise point positioning with GPS and BeiDou   总被引：2，自引：1，他引：1  

Li Pan  Zhang Xiaohong  Guo Fei 《Journal of Geodesy》2017,91(1):25-40

This paper focuses on the contribution of the global positioning system (GPS) and BeiDou navigation satellite system (BDS) observations to precise point positioning (PPP) ambiguity resolution (AR). A GPS + BDS fractional cycle bias (FCB) estimation method and a PPP AR model were developed using integrated GPS and BDS observations. For FCB estimation, the GPS + BDS combined PPP float solutions of the globally distributed IGS MGEX were first performed. When integrating GPS observations, the BDS ambiguities can be precisely estimated with less than four tracked BDS satellites. The FCBs of both GPS and BDS satellites can then be estimated from these precise ambiguities. For the GPS + BDS combined AR, one GPS and one BDS IGSO or MEO satellite were first chosen as the reference satellite for GPS and BDS, respectively, to form inner-system single-differenced ambiguities. The single-differenced GPS and BDS ambiguities were then fused by partial ambiguity resolution to increase the possibility of fixing a subset of decorrelated ambiguities with high confidence. To verify the correctness of the FCB estimation and the effectiveness of the GPS + BDS PPP AR, data recorded from about 75 IGS MGEX stations during the period of DOY 123-151 (May 3 to May 31) in 2015 were used for validation. Data were processed with three strategies: BDS-only AR, GPS-only AR and GPS + BDS AR. Numerous experimental results show that the time to first fix (TTFF) is longer than 6 h for the BDS AR in general and that the fixing rate is usually less than 35 % for both static and kinematic PPP. An average TTFF of 21.7 min and 33.6 min together with a fixing rate of 98.6 and 97.0 % in static and kinematic PPP, respectively, can be achieved for GPS-only ambiguity fixing. For the combined GPS + BDS AR, the average TTFF can be shortened to 16.9 min and 24.6 min and the fixing rate can be increased to 99.5 and 99.0 % in static and kinematic PPP, respectively. Results also show that GPS + BDS PPP AR outperforms single-system PPP AR in terms of convergence time and position accuracy.  相似文献   

西风槽与副高相互作用的暴雨过程动热力场结构特征分析   总被引：2，自引：2，他引：0  

侯淑梅  郭俊建  张磊  郑怡  孙兴池 《气象》2017,43(2):151-165

利用常规气象观测、自动气象站加密观测、NCEP/NCAR(1°×1°,逐6 h)再分析以及FY 2C卫星云图等资料,分析了2007年8月15—18日发生在山东的一次暴雨过程中,西风槽与副热带高压(以下简称副高)相互作用三个阶段的热力、动力场结构特征。结果表明:整个过程先后经历了副高西进切变线缓慢西移、横槽南压副高减弱和横槽转竖副高南撤三个阶段,三个阶段的共同特征是中低层有切变线和θ_(se)锋区;700 hPa有低空急流;产生暴雨的对流云团具有后向传播特征,生命史中多次发生合并。三个阶段的不同点是:(1)副高西进过程中,锋区随高度向北倾斜,坡度小,切变线和θ_(se)锋区均为后倾,为典型的暖锋降水。暴雨区范围大,强度均匀,位于850 hPaθ_(se)锋区与暖脊的交界处的水汽辐合中心附近。饱和区宽广,伸展高度高。低层气旋性辐合、切变线辐合、锋面抬升是触发暴雨的动力机制,低空急流是暴雨增强机制。(2)副高减弱过程中,干冷空气分别从低层和中层侵入θ_(se)暖脊,θ_(se)锋区随高度先向北后向南,呈交错倾斜现象,坡度大,为典型的强对流降水,上升运动最为激烈。暴雨区范围小,强度大,分布不均,位于θ_(se)暖脊垂直方向轴线附近。饱和区狭窄,伸展高度高。锋面抬升运动是触发对流性强降水的主要动力机制,对流层中层干冷空气入侵是强降水的增强机制。(3)副高南撤过程中,θ_(se)锋区随高度向南倾斜,坡度大,呈前倾特征,为典型的高空槽降水。暴雨区狭长分散,强度弱,位于850 hPa切变线上、θ_(se)暖舌靠近锋区一侧。饱和区狭窄,伸展高度低。低层切变线辐合抬升是触发强降水动力机制,中层干侵入是降水增强机制。  相似文献   

BS-ACEBOC: a generalized low-complexity dual-frequency constant-envelope multiplexing modulation for GNSS     

Guo  Fu  Yao  Zheng  Lu  Mingquan 《GPS Solutions》2017,21(2):561-575

GPS Solutions - In order to satisfy the need for combining signals in a constant-envelope modulation, we propose a new dual-frequency constant-envelope modulation (DCEM), called asymmetric...  相似文献   

Enhanced orbit determination for BeiDou satellites with FengYun-3C onboard GNSS data     

Zhao  Qile  Wang  Chen  Guo  Jing  Yang  Guanglin  Liao  Mi  Ma  Hongyang  Liu  Jingnan 《GPS Solutions》2017,21(3):1179-1190

GPS Solutions - A key limitation for precise orbit determination of BeiDou satellites, particularly for satellites in geostationary orbit (GEO), is the relative weak geometry of ground stations....  相似文献   

Mining parameter information for building extraction and change detection with very high-resolution imagery and GIS data     

Zhou Guo 《地理信息系统科学与遥感》2017,54(1):38-63

  相似文献   

基于GIS的承德乡村地名文化景观空间分布特征   总被引：4，自引：2，他引：2  

孙百生  郭翠恩  杨依天  葛伟 《地理科学》2017,37(2):244-251

将承德地区乡村地名作为离散点,以GIS中移动搜索法的点距离空间平滑分析法为支撑,从地理区域这一角度分析地名文化景观空间分布特征。研究发现：承德地区自然类景观,以“山”、“水文”、“动植物”命名的地名分布主要位于中低海拔高度的平坦地区;承德地区乡村地名文化景观划分为军事活动类、经济活动类、房屋建筑类、美愿与纪念类、满蒙少数民族语言及方言类,其空间分布特征与当地历史时期的军事、生产生活、社会变迁的相对频繁程度以及人口稠密情况基本上相符合。  相似文献   

长江经济带工业废水排放的时空格局演化及驱动因素   总被引：7，自引：2，他引：5  

陈昆仑  郭宇琪  刘小琼  张祚 《地理科学》2017,37(11):1668-1677

利用探索性空间分析方法（ESDA）和迪氏分解模型（LMDI）研究长江经济带2002~2013年工业废水排放的时空格局演化和主要驱动因素。① 时空格局演化方面,时间上工业废水排放先上升后下降,在2005年达到峰值。空间上,排放量自上游向下游增加;高排放城市减少,中排放城市增多;工业废水排放自下游向中上游转移,并由大城市向中小城市扩散;呈现明显的空间集聚状态。② 驱动因素方面,经济发展效应和技术进步效应分别是工业废水排放增多和降低的主导因素;产业结构效应的影响取决于产业发展政策的调整;人口规模效应影响较小。  相似文献