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91.
确定局部高程基准相对大地水准面的垂直偏差是统一全球高程基准的重要途径。本文的目的是通过大港验潮站坐标直接确定我国高程基准的垂直偏差。首先给出通过大港验潮站坐标确定我国高程基准垂直偏差的基本原理,然后介绍测定大港验潮站平均海面坐标的方法及过程,接下来通过EGM2008和EIGEN-6C4重力场模型计算出的我国高程基准面的重力位,进而推算获得垂直偏差,并与我国东部地区GPS/水准数据的计算结果进行了比较。经分析发现,EGM2008模型计算结果的可靠性要好于EIGEN-6C4模型;利用大港验潮站坐标计算得到的我国高程基准相对大地水准面的垂直偏差为0.344 m,比利用我国东部261个GPS/水准点数据计算获得的偏差值小0.006 m。 相似文献
92.
The marine environmental forecast plays an increasingly important role in economic growth and infrastructure development, and touches upon many fields and aspects, including marine security, energy resources development and protection, ocean shipping and fisheries. Global Ocean Data Assimilation Experiment (GODAE) OceanView supports the national research groups providing them with coordination and technical support among the partners. Forecasting centers develop and establish global operational ocean forecast systems. The global operational ocean forecasting system uses the ocean dynamic numerical model as the dynamic framework, and the near real-time high-quality observation input field is integrated into the model by data assimilation to realize the future environmental forecasts of the marine conditions covering the multi-time scale. The products are routinely validated with observations in order to assess their quality. This paper briefly introduced and reviewed the development process and current situation of the global ocean forecasting system covered by GODAE OceanView, and outlined the future development of global ocean forecasting. 相似文献
93.
在无标样条件下 ,我们利用微束 X荧光分析法对南极乔治王岛的 6种苔藓植物的叶和茎进行重元素分析。它们是 :Andreaea regularis,Bryum muehlenbeckii,Drepanocladus uncinatus,Brachythecium subpilosum,Tortula saxiola,Ditrichum austro- georgicum。研究结果发现 ,不同苔藓植物对各种不同重元素的吸收能力不同 ,即使是同一种植物 ,叶和茎中的重元素成分也有差异。在 6种苔藓中 ,Andreaea regularis体内的重元素种类最少 ,但其对 Fe有较强的吸收。由于南极环境条件优越 ,在苔藓植物体内 ,尚未发现大量有毒重金属元素的存在 相似文献
94.
CGCS2000高精度坐标转换格网模型的建立 总被引:1,自引:0,他引:1
CGCS2000启用后,用于地形图图廓线和坐标网变换的高精度坐标转换格网模型的建立成为实用中的重要问题。本文阐述我国CGCS2000高精度坐标转换格网模型的建立方法。一是讨论坐标转换最小曲率方程,该方程同时具备整体光滑和局部光滑特性,可以更好地符合地图线状要素坐标转换时的连续光滑性;二是提出格网节点迭代计算方法以及拟合推估两步极小法构建区域性格网模型的方法,构建了格网模型数据结构;三是给出全国范围CGCS2000高精度坐标转换格网模型的最优格网间距和转换精度,按48 433个2000国家大地控制网点坐标构建了BJS54和XAS80到CGCS2000坐标转换格网模型,转换后的点位外符精度分别为0.26m和0.03m。 相似文献
95.
Evolution of an anticyclonic eddy southwest of Taiwan 总被引:8,自引:1,他引:7
Tingting Zu Dongxiao Wang Changxiang Yan Igor Belkin Wei Zhuang Ju Chen 《Ocean Dynamics》2013,63(5):519-531
Satellite images of sea-surface temperature, surface chlorophyll a concentration, and sea-level anomaly, together with ocean reanalysis data of Asia and Indian–Pacific Ocean (AIPOcean1.0), are utilized to study the three-dimensional characteristics and evolution of an anticyclonic warm eddy adjacent to the southwest coast of Taiwan during October and November 2006. Originated from the Kuroshio intrusion in the Luzon Strait, but unlike previously found westward moving anticyclonic eddies (AE) in the northeastern South China Sea, this AE was so close to the Taiwan coast and stayed where it was formed for over 1 month until it dissipated. Energy analysis is utilized to study the evolution process of the AE, and it shows that the barotropic instability (BTI) and baroclinic instability introduced by the Kuroshio intrusion flow appear to be the main energy sources for the AE. Periodical enhancement/relaxation of local northeasterly monsoon and its associated negative wind stress curl modify the current patterns in this region, reinforce the intraseasonal variability of the Kuroshio intrusion flow, and act together with Kuroshio to form the AE. Eddies detected from AIPOcean1.0 data also show that AEs are most likely to be generated southwest of Taiwan during the transition period of summer monsoon to winter monsoon, and generally, the BTI of Kuroshio intrusion contributes more than the direct wind stress work to the increase of the eddy kinetic energy for the generation and growth of the AEs. 相似文献
96.
长期的露天开采严重破坏了矿山地理地质环境,产生了地质灾害隐患。在介绍矿区地理地质背景的基础上,系统地描述该矿区土地、植被、地形和地貌被破坏的情况,分析崩塌、滑坡和泥石流地质灾害隐患。为改善生态环境,打造全国知名旅游景区,提出全面停止矿山开采,并进行分期治理。先期重点清除存在隐患的废石堆,然后清除边坡破碎危岩体,并辅以绿化措施。 相似文献
97.
98.
The thermocline-sea surface temperature (SST) feedback is the most important component of the Bjerknes feedback, which plays an important role in the development of the air-sea coupling modes of the Indian Ocean. The thermocline-SST feedback in the Indian Ocean has experienced significant decadal variations over the last 40 a. The feedback intensified in the late twentieth century and then weakened during the hiatus in global warming at the early twenty-first century. The thermocline-SST feedback is most prominent in the southeastern and southwestern Indian Ocean. Although the decadal variations of feedback are similar in these two regions, there are still differences in the underlying mechanisms. The decadal variations of feedback in the southeastern Indian Ocean are dominated by variations in the depth of the thermocline, which are modulated by equatorial zonal wind anomalies. Whereas the decadal variation of feedback in the southwestern Indian Ocean is mainly controlled by the intensity of upwelling and thermocline depth in winter and spring, respectively. The upwelling and thermocline depth are both affected by wind stress curl anomalies over the southeastern Indian Ocean, which excite anomalous Ekman pumping and influence the southwestern Indian Ocean through westward propagating Rossby waves. 相似文献
99.
Ang Li Xueming Zhu Yunfei Zhang Shihe Ren Miaoyin Zhang Ziqing Zu Hui Wang 《海洋学报(英文版)》2021,40(11):87-103
In order to satisfy the increasing demand for the marine forecasting capacity, the Bohai Sea, the Yellow Sea and the East China Sea Operational Oceanography Forecasting System (BYEOFS) has been upgraded and improved to Version 2.0. Based on the Regional Ocean Modeling System (ROMS), a series of comparative experiments were conducted during the improvement process, including correcting topography, changing sea surface atmospheric forcing mode, adjusting open boundary conditions, and considering atmospheric pressure correction. (1) After the topography correction, the volume transport and meridional velocity maximum of Yellow Sea Warm Current increase obviously and the unreasonable bending of its axis around 36.1°N, 123.5°E disappears. (2) After the change of sea surface forcing mode, an effective negative feedback mechanism is formed between predicted sea surface temperature (SST) by the ocean model and sea surface radiation fluxes fields. The simulation errors of SST decreased significantly, and the annual average of root-mean-square error (RMSE) decreased by about 18%. (3) The change of the eastern lateral boundary condition of baroclinic velocity from mixed Radiation-Nudging to Clamped makes the unreasonable westward current in Tsushima Strait disappear. (4) The adding of mean sea level pressure correction option which forms the mean sea level gradient from the Bohai Sea and the Yellow Sea to the western Pacific in winter and autumn is helpful to increasing the fluctuation of SLA and outflow of the Yellow Sea when the cold high air pressure system controls the Yellow Sea area. 相似文献
100.
不同扰动方式对沙砾质戈壁地表风蚀量的影响 总被引:2,自引:1,他引:1
通过野外风洞实验,测定了不同破坏方式、破坏面积和风速下的沙砾质戈壁风蚀量。结果表明:不同破坏方式引起的风蚀量不同,扰动强度越大造成的风蚀量越多;相同扰动方式下连续破坏造成的风蚀量稍高于间隔破坏。风蚀总量随破坏面积的增大而增加,且服从指数函数。风速为8~10 m·s-1时,扰动的戈壁地表以轻微侵蚀为主;10~12 m·s-1 是风蚀量增幅最大阶段;当风速大于 12 m·s-1时,以强烈风蚀为主。风沙流中沙物质的主体是细沙和极细沙,在20 cm高度范围内,自风沙流下层至上层细沙含量比较稳定,极细沙含量逐渐降低,中沙含量逐渐上升。 相似文献