Climate-driven trends and ecological implications of event-scale upwelling in the California Current System

被引:74
作者
Iles, Alison C. [1 ]
Gouhier, Tarik C. [1 ]
Menge, Bruce A. [1 ]
Stewart, Julia S. [2 ]
Haupt, Alison J. [3 ]
Lynch, Margaret C. [4 ]
机构
[1] Oregon State Univ, Dept Zool, Corvallis, OR 97331 USA
[2] Stanford Univ, Hopkins Marine Stn, Pacific Grove, CA 93950 USA
[3] Calif Nat Resources Agcy, Sacramento, CA 95814 USA
[4] Univ Virginia, Sch Med, Charlottesville, VA 22908 USA
基金
美国安德鲁·梅隆基金会; 加拿大自然科学与工程研究理事会; 美国国家科学基金会;
关键词
California Current System; climate change; coastal ecosystem; environmental forcing; recruitment; rocky intertidal; upwelling; CROSS-SHELF TRANSPORT; BARNACLE SETTLEMENT; FAVORABLE WINDS; SURF ZONE; RECRUITMENT; COASTAL; TEMPERATURE; POPULATIONS; RESPONSES; LARVAE;
D O I
10.1111/j.1365-2486.2011.02567.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Eastern boundary current systems are among the most productive and lucrative ecosystems on Earth because they benefit from upwelling currents. Upwelling currents subsidize the base of the coastal food web by bringing deep, cold and nutrient-rich water to the surface. As upwelling is driven by large-scale atmospheric patterns, global climate change has the potential to affect a wide range of significant ecological processes through changes in water chemistry, water temperature, and the transport processes that influence species dispersal and recruitment. We examined long-term trends in the frequency, duration, and strength of continuous upwelling events for the Oregon and California regions of the California Current System in the eastern Pacific Ocean. We then associated event-scale upwelling with up to 21 similar to years of barnacle and mussel recruitment, and water temperature data measured at rocky intertidal field sites along the Oregon coast. Our analyses suggest that upwelling events are changing in ways that are consistent with climate change predictions: upwelling events are becoming less frequent, stronger, and longer in duration. In addition, upwelling events have a quasi-instantaneous and cumulative effect on rocky intertidal water temperatures, with longer events leading to colder temperatures. Longer, more persistent upwelling events were negatively associated with barnacle recruitment but positively associated with mussel recruitment. However, since barnacles facilitate mussel recruitment by providing attachment sites, increased upwelling persistence could have indirect negative impacts on mussel populations. Overall, our results indicate that changes in coastal upwelling that are consistent with climate change predictions are altering the tempo and the mode of environmental forcing in near-shore ecosystems, with potentially severe and discontinuous ramifications for ecosystem structure and functioning.
引用
收藏
页码:783 / 796
页数:14
相关论文
共 71 条
[1]  
Atlas E.L., 1971, A practical manual for the use of the Technicon Autoanalyzer in seawater nutrient analysis (revised)
[2]   GLOBAL CLIMATE CHANGE AND INTENSIFICATION OF COASTAL OCEAN UPWELLING [J].
BAKUN, A .
SCIENCE, 1990, 247 (4939) :198-201
[3]  
BAKUN A, 1974, FISH B-NOAA, V72, P843
[4]   Greenhouse gas, upwelling-favorable winds, and the future of coastal ocean upwelling ecosystems [J].
Bakun, Andrew ;
Field, David B. ;
Redondo-Rodriguez, Ana ;
Weeks, Scarla J. .
GLOBAL CHANGE BIOLOGY, 2010, 16 (04) :1213-1228
[5]   Time-dependent, wind-driven flow over a shallow midshelf submarine bank [J].
Barth, JA ;
Pierce, SD ;
Castelao, RM .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2005, 110 (C10) :1-20
[6]  
Berlow EL, 1997, ECOL MONOGR, V67, P435, DOI 10.1890/0012-9615(1997)067[0435:FCTCHE]2.0.CO
[7]  
2
[8]   Spatial and temporal patterns of invertebrate recruitment along the West Coast of the United States [J].
Broitman, B. R. ;
Blanchette, C. A. ;
Menge, B. A. ;
Lubchenco, J. ;
Krenz, C. ;
Foley, M. ;
Raimondi, P. T. ;
Lohse, D. ;
Gaines, S. D. .
ECOLOGICAL MONOGRAPHS, 2008, 78 (03) :403-421
[9]  
Brown JH, 2004, ECOLOGY, V85, P1771, DOI 10.1890/03-9000
[10]   Coastal ocean response to summer upwelling favorable winds in a region of alongshore bottom topography variations off Oregon [J].
Castelao, RM ;
Barth, JA .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2005, 110 (C10) :1-17