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与 sea level 相关的网络例句 [注:此内容来源于网络,仅供参考]

A new index is developed for land-sea thermal difference zonally/meridionally in terms of east Asian zonal sea-level pressure difference combined with high and low-level zonal wind shear at low latitudes.

将东亚纬向海平面气压差与低纬度高低层纬向风切变结合,定义了一个能表征东西和南北向海陆热力差异的东亚季风指数。

Persculptus to Parakidograptus acuminatus Zones, could be recognized during the interval. In addition, the abundance changes of the radiolaria at the Goujiaya and Datangkou sections were coincided with the sea-level changes, and correlatable with the synchorous 5 fluctuations of the sea-level in North America and Africa. So above-mentioned 5 cycles could represent the eustasies during the latest Ordovician to the earliest Silurian.

在这2个剖面上,放射虫丰度变化也表现出相似的规律,与笔石和腕足类的形态、分异度和丰度变化所反应的海平面升降大体一致,和北美、非洲同期海平面的5次波动可以对比,据此指出,以上5次海平面旋回代表了晚奥陶世晚期至志留纪初期全球性海平面变化。

Persculptus to Parakidograptus acuminatus Zones, could be recognized during theinterval. In addition, the abundance changes of the radiolaria at the Goujiaya and Datangkou sections werecoincided with the sea-level changes, and correlatable with the synchorous 5 fluctuations of the sea-level inNorth America and Africa. So above-mentioned 5 cycles could represent the eustasies during the latestOrdovician to the earliest Silurian.

在这2个剖面上,放射虫丰度变化也表现出相似的规律,与笔石和腕足类的形态、分异度和丰度变化所反应的海平面升降大体一致,和北美、非洲同期海平面的5次波动可以对比,据此指出,以上5次海平面旋回代表了晚奥陶世晚期至志留纪初期全球性海平面变化。

Eustatic sea level change; fluctuation of sea level

由于热膨胀、冰盖在温暖条件下的消融或在寒冷条件下的扩张而引起的相对海平面的长期变化。

With the seismic profile and the comparison between the eustatic sea level change and sequence, the authors find that there developed different scales of reef and carbonate platforms in the sag. These reef and carbonate platforms have many developing stages which can be correlated with the eustatic sea level change and evolutionary stages, besides, they all have preferable hydrocarbon potential.

通过地震资料的解释及海平面变化曲线与层序的对比发现,琼东南盆地南部深水凹陷发育有规模大小不等的生物礁和碳酸盐岩台地,而且这些生物礁和碳酸盐岩台地的发育与海平面变化曲线和构造演化的阶段可以对应起来,应具有较好的油气勘探潜力。

Study shows that environment evolution and eustatic change of Holocene in this area may be divided into 6 stages:① early stage of early Holocene, 9 100~10 900 aBP,when sea level was low and this area was an oxidizing environment or oxidizing-reducing transition environment;② late stage of early Holocene, 8 000~9 100 aBP, sea-level rising,...

研究表明,本区全新世环境演化分为6个阶段:①早全新世早期,10900~9100aBP,海平面较低,尚未淹没本区,为近岸氧化环境或氧化—还原过渡环境;②早全新世晚期,9100~8000aBP,海水上涨,本区时淹时退,为浅海或潮坪环境,生物钻孔发育;③中全新世主体,8000~4150aBP,海平面快速上升,完全淹没,Fe2+/Fe3+介于0.7395~1.9123之间,为全新世中最高段,表明还原程度强、全球气候变暖;④中全新世后期,4150~2850aBP,海水有所下降,仍为浅海环境,Fe2+/Fe3+较高,多在1.0以上;⑤晚全新世,2850~1310aBP,海平面进一步下降,本区时常暴露,其中2150~1310aBP以还原环境为主,为潮下带,2150~2850aBP以氧化—还原过渡环境为主,为潮间带;⑥1855AD以来,海平面基本稳定,稍有上升,为现代黄河三角洲沉积时期。本区全新世至少存在5期冷热交替的旋回性气候变化。

The lowest point is sea level, while the highest point is in Chestnut Hill, at approximately 445 feet (136 m) above sea level (near the intersection of Germantown Avenue and Bethlehem Pike).

最低点是海平面,而最高点是在栗山,大约四百四十五英尺( 136米)海平面以上(接近交叉杰曼大道和伯利恒派克)。

Miller, a paleobiologist and professor of geology at the University of Cincinnati, says the new study is striking because it establishes a clear relationship between the tempo of mass extinction events and changes in sea level and sediment: Over the years, researchers have become fairly dismissive of the idea that marine mass extinctions like the great extinction of the Late Permian might be linked to sea-level declines, even though these declines are known to have occurred many times throughout the history of life.

&阿诺德一Miller表示,与古地质学教授在辛辛那提大学说,新研究是惊人的,因为它确立了明确的关系节奏的大规模灭绝事件和海平面变化和沉积物:&多年来,研究人员已成为相当不屑一顾的想法,海洋生物大灭绝一样伟大的濒临灭绝的晚二叠世可能与海平面下降,即使这些下降是众所周知的已经发生很多次整个生命的历史。清楚这项研究的关系文件将促使许多人重新考虑其以前的意见。

The atmospheric pressure at the top of Everest is about a third of sea level pressure, implicating that there is about a third as much oxygen available to breathe as at sea level.

在珠穆朗玛峰最高处的大气压约为海平面气压的三分之一,即意味着,在那里大约只有海平面的三分之一多的氧气可供呼吸。

After analyzing the impacting factors of natural vulnerability along the Pearl River mouth, the paper divides the coastline of approximately 412km into 25 15-minute gird cells. For assessment purposes, the six variables including geography, relative sea-level change, average tide range, regional slope, shoreline erosion or accretion rates and tropic cyclone impacting frequency are selected as assessed variables. Once each section of coastline is assigned a risk value for each specific data variable, the costal vulnerability index can be useto calculate the natural vulnerability of the areas along the Pearl River mouth. After that, the paper develops a database for assessment of coastal vulnerability to sea-level rises and protracts a 1:2,000,000 vectors CVI map of the coastlines along the Pearl River mouth.

为了探讨不同海岸带对未来海平面上升的自然脆弱性,本文以珠江口沿岸作为研究个案,在分析珠江口沿岸自然脆弱性的影响因子的基础上,把珠江口沿岸412km岸线划分为25个15′×15′的网格单元,选取了地质、海平面上升率、平均潮差、区域海岸坡度、海岸侵蚀/堆积率、热带气旋影响频率6个评价指标,应用CVI指数评价公式对珠江口地区进行海岸脆弱性评价,并建立海岸脆弱性评价数据库,绘制了珠江口沿岸1:2,000,000的数字化CVI图。

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