sea level change

基本解釋

Relative sea level change is controlled by global sea-level and various regional factors, such as land sink and atmospheric pressures.
相對海面變化是由全球絕對海面變化和區(qū)域性地面和海面因素共同控制。
Such rates of sea level change have occurred many times in Earth's history in response to global warming rates no higher than those of the past 30 years.
這種速率的海平面變化在地球史上并不乏先例，但作為誘因的全球變暖速率還沒有哪一次能像過去 30年這么高的。
The sea level change curves in varied epochs of the Devonian are given, which are essentially in accord with the global sea level change curves of Devonian shelf sedimentary environments.
該區(qū)泥盆紀(jì)不同時(shí)期的海平面變化曲線與全球泥盆紀(jì)陸棚沉積環(huán)境海平面變化曲線總體趨勢基本一致。

However, the peak volcanism trailed behind the highest rates of sea level change by around 4, 000 years.
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Melott says that although the Northern hemisphere would have been left untouched by the first pulse of the extinction, he notes that, later, glaciation and sea level change would have had an impact everywhere.
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Problems arise from conflicts between different uses of coastal land and waters, overexploitation of coastal resources, discharge of wastes and effluents into coastal waters, increasing stress by sea level change and growth of coastal population.
UNESCO: Water Portal