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Long-term observations of deepwater renewal in Crater Lake, Oregon

机译:俄勒冈火山口湖深水更新的长期观测

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We examine observations of key Iimnological properties (primarily temperature, salinity, and dissolved oxygen), measured over a 14-year period in Crater Lake, Oregon, and discuss variability in the hypolimnion on time scales of days to a decade. During some years (e.g., 1994-1995), higher-than-average wintertime deep convection and ventilation led to the removal of significant amounts of heat and salt from the hypolimnion, while dissolved oxygen concentrations increase. In other years, suchas the winter of 1996-1997, heat and salt concentrations increase throughout the year and dissolved oxygen levels drop, indicating conditions were dominated by the background geothermal inputs and dissolved oxygen consumption by bacteria (i.e., minimaldeep convection). Over the entire 14 year period, no statistically significant trend was observed in the annual hypolimnetic heat and salt content. Measurements from several thermistors moored in the hypolimnion provide new insight into the time and space scales of the deep convection events. For some events, cool water intrusions are observed sequentially, from shallower depths to deeper depths, suggesting vertical mixing or advection from above. For other events, the cooling is observed first at the deepest sensors, suggesting a thin, cold water pulse that flows along the bottom and mixes more slowly upwards into the basin. In both cases, the source waters must originate from the epilimnion. Conditions during a strong ventilation year (1994-1995) and a weak ventilation year (1996-1997) were compared. The results suggest the major difference between these 2 years was the evolution of the stratification in the epilimnion during the first few weeks of reverse stratification such that thermobaric instabilities were easier to form during 1995 than 1997. Thus, the details of surface cooling and wind-driven mixing during the early stages of reverse stratification may determine the net amount of ventilation possible during a particular year.
机译:我们检查了在俄勒冈州Crater Lake的14年期间内测得的主要昆虫学特性(主要是温度,盐度和溶解氧)的观察结果,并讨论了在几天到十年的时间尺度上的次生动物的变化。在某些年中(例如1994-1995年),冬季深对流和通风高于平均水平,导致从次高纯棉中除去了大量的热量和盐分,而溶解氧的浓度却增加了。在其他年份中,例如1996-1997年的冬天,全年热量和盐浓度增加,溶解氧水平下降,这表明条件主要是背景地热输入和细菌溶解氧消耗(即最小对流)。在整个14年的时间里,年度低铁热和盐含量均未观察到统计学上的显着趋势。来自停泊在下斜层中的几个热敏电阻的测量结果为深对流事件的时间和空间尺度提供了新的见解。对于某些事件,从较浅的深度到较深的深度依次观察到冷水侵入,表明从上方垂直混合或对流。对于其他事件,首先在最深处的传感器处观察到冷却,这表明有细的冷水脉冲沿底部流动,并向上缓慢混合进入盆地。在这两种情况下,源水都必须来自the水。比较了强通风年(1994-1995年)和弱通风年(1996-1997年)的状况。结果表明,这两年之间的主要区别在于逆分层的最初几周,上层层的分层演化,使得1995年比1997年更容易形成热压不稳定性。因此,地表冷却和风的细节在逆向分层的早期阶段进行混合驱动可能会确定特定年份可能的净通风量。

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