You are a guest now, please register and log in above
This system will translate non-English text to standard English, or help correct your English writing's spelling, grammar, and syntax errors, and rewrite out as professional scientific English.
《以下原始文字来自公开网站》 more examples
例-1 中翻英
Input：海洋流动对海洋物质、能量、热量和淡水等的输运起着至关重要的作用，对海洋生态环境和气候变化有着重要的影响，因此，海洋流动的量化一直是海洋观测和研究的核心问题之一。目前广泛使用的海面流场信息，是来自于利用地转平衡假设、从卫星高度计的海面高度资料中获取海面地转流场的数据。经典的地转平衡假设是基于地球旋转诱导的科氏力和压强梯度力之间的平衡，忽略了流动的曲率影响。然而海洋充满了中小尺度涡旋和流线弯曲的现象，考虑曲率的影响将会从高度计资料中获取额外的流动信息。
Output： Ocean currents play a crucial role in the transport of oceanic substances, energy, heat, and freshwater, and have significant impacts on the marine ecological environment and climate change. Therefore, the quantification of ocean currents has always been one of the core issues in ocean observation and research. Currently, widely used sea surface flow field information is obtained from the data of sea surface geostrophic flow field using the assumption of geostrophic balance and satellite altimetry data. The classical assumption of geostrophic balance is based on the balance between the Coriolis force induced by the rotation of the Earth and the pressure gradient force, neglecting the curvature effect of the flow. However, the ocean is full of phenomena such as mesoscale eddies and curved streamlines, and considering the effect of curvature will provide additional flow information from altimetry data.
Example-2 correct and improve English
Input： The Last Deglacial (~19 ka BP ~ 11.5 ka BP) is the time period of the transition from the last major ice age to the warm period in the evolution of the Earth's climate, the study of its climate evolution mechanism can help to better understand the transition mechanism of the Earth's climate from cold to warm and provide a reference to cope with the current global warming.
However, a difficult problem in the study of climate evolution during the Last Deglacial is to decipher the interaction mechanisms between the atmospheric and oceanic climate systems.
Recently, the research team led by Prof. Wan from the Institute of Oceanology of the Chinese Academy of Sciences (IOCAS) reported a foraminiferal neodymium (Nd) isotopic record spanning the past 17,000 years with an unprecedented resolution of 200 years. This record used a mid-water marine core from the northern Indian Ocean to compare the differing interhemispheric relationships between the Indian Summer Monsoon and Antarctic Intermediate Water (AAIW).
Output： The Last Deglacial period, which occurred approximately 19,000 to 11,500 years ago, marks the transition from the last major ice age to a warmer period in Earth's climate evolution. Understanding the mechanisms behind this transition can provide valuable insights into the current global warming crisis. However, a significant challenge in studying climate evolution during this period is deciphering the complex interactions between atmospheric and oceanic climate systems.
Recently, a research team led by Professor Wan from the Institute of Oceanology of the Chinese Academy of Sciences (IOCAS) reported a neodymium (Nd) isotopic record of foraminifera spanning the past 17,000 years with an unprecedented resolution of 200 years. This record was obtained from a mid-water marine core in the northern Indian Ocean and was used to compare the interhemispheric relationships between the Indian Summer Monsoon and Antarctic Intermediate Water (AAIW).
例-3 中翻英
Input：为深入认识洪季特枯水情下长江流域-河口-近海系统物质通量演化及生态环境响应，加强陆海相互作用的河口海岸的系统性研究，河口海岸学国家重点实验室组织多学科、多专业和多手段综合调查团队，于2022年12月开展了长江中下游水沙、地貌、地质、水质、生态和微塑料的综合调查。
2022年长江中下游经历了历史性的洪季特枯水情，大通站径流9月底已降至常年枯季流量低值的10000 m3/s以下，三峡水库蓄水仅至159 m，如此长的枯水期，对长江、长江口及近海海域的影响值得关注。本次长江流域综合调查，针对全球变化背景下河口海岸水沙地貌和生态环境系统面临的挑战，结合长江上游梯级水库群建设、中下游河道普遍面临冲刷及泥沙格局转换等现状，围绕“流域-河口-近海系统物质通量演化及生态环境响应”问题而开展综合调查。
Output：
In order to gain a deeper understanding of the evolution of material flux and ecological responses in the Yangtze River Basin-estuary-nearshore system under the conditions of the Hongji drought, and to strengthen the systematic research on the land-sea interaction of the estuarine coast, the State Key Laboratory of Estuarine and Coastal Research organized a multidisciplinary, multi-professional, and multi-method comprehensive survey team in December 2022 to conduct a comprehensive survey of water and sediment, landforms, geology, water quality, ecology, and microplastics in the middle and lower reaches of the Yangtze River.
In 2022, the middle and lower reaches of the Yangtze River experienced a historic flooding-season drought, with the flow at the Datong station dropping below 10,000 m3/s, the lowest value for the dry season, by the end of September. The Three Gorges Reservoir only reached a storage level of 159 m. Such a long drought period deserves attention for its impact on the Yangtze River, the Yangtze River estuary, and the adjacent nearshore waters. In this comprehensive survey of the Yangtze River Basin, in the context of global change, the challenges faced by the water and sediment, landforms, and ecological environment systems of the estuarine coast were addressed, taking into account the construction of the cascade reservoirs in the upper reaches of the Yangtze River, the erosion and sediment pattern changes in the middle and lower reaches of the river, and other current situations. The survey was conducted around the issue of 'evolution of material flux and ecological responses in the Yangtze River Basin-estuary-nearshore system.'