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

被引:27
作者
Crawford, G. B.
Collier, R. W.
机构
[1] Humboldt State Univ, Dept Oceanog, Arcata, CA 95521 USA
[2] Oregon State Univ, Coll Ocean & Atmospher Sci, Corvallis, OR 97331 USA
关键词
hypolimnion; vertical mixing; nutrient upwelling; ventilation; cold-water intrusions; interannual variability; long-term monitoring; climate change;
D O I
10.1007/s10750-006-0345-3
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
We examine observations of key limnological 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, such as 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., minimal deep 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 1995-1997. 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.
引用
收藏
页码:47 / 68
页数:22
相关论文
共 43 条
[1]   Energetics of long internal gravity waves in large lakes [J].
Antenucci, JP ;
Imberger, J .
LIMNOLOGY AND OCEANOGRAPHY, 2001, 46 (07) :1760-1773
[2]  
Bacon C. R., 1990, CRATER LAKE ECOSYSTE, P19
[3]  
Bacon CR, 2002, GEOL SOC AM BULL, V114, P675, DOI 10.1130/0016-7606(2002)114<0675:MVAMWI>2.0.CO
[4]  
2
[5]   THE CONCENTRATION AND ISOTOPIC FRACTIONATION OF OXYGEN DISSOLVED IN FRESH-WATER AND SEAWATER IN EQUILIBRIUM WITH THE ATMOSPHERE [J].
BENSON, BB ;
KRAUSE, D .
LIMNOLOGY AND OCEANOGRAPHY, 1984, 29 (03) :620-632
[6]  
CARMACK EC, 1991, ELSEV OCEANOGR SERIE, V57, P215, DOI 10.1016/S0422-9894(08)70069-2
[7]  
CARPENTER JAMES H., 1965, LIMNOL OCEANOGR, V10, P135
[8]  
CARPENTER JAMES H., 1965, LIMNOL OCEANOGR, V10, P141
[9]   PRECISE THERMODYNAMIC PROPERTIES FOR NATURAL-WATERS COVERING ONLY THE LIMNOLOGICAL RANGE [J].
CHEN, CTA ;
MILLERO, FJ .
LIMNOLOGY AND OCEANOGRAPHY, 1986, 31 (03) :657-662
[10]   Observations of a deep-mixing event in Crater Lake, Oregon [J].
Crawford, GB ;
Collier, RW .
LIMNOLOGY AND OCEANOGRAPHY, 1997, 42 (02) :299-306