Atmospheric consequences of disruption of the ocean thermocline

被引:11
|
作者
Kwiatkowski, Lester [1 ]
Ricke, Katharine L. [1 ]
Caldeira, Ken [1 ]
机构
[1] Carnegie Inst Sci, Dept Global Ecol, Stanford, CA 94305 USA
来源
ENVIRONMENTAL RESEARCH LETTERS | 2015年 / 10卷 / 03期
关键词
biogeochemistry; oceanography; ocean pipes; thermocline; CLIMATE FEEDBACK PROCESSES; FUTURE CHANGES; ENERGY; SENSITIVITY; EARTH; CURE;
D O I
10.1088/1748-9326/10/3/034016
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Technologies utilizing vertical ocean pipes have been proposed as a means to avoid global warming, either by providing a source of clean energy, increasing ocean carbon uptake, or storing thermal energy in the deep ocean. However, increased vertical transport of water has the capacity to drastically alter the ocean thermocline. To help bound potential climate consequences of these activities, we perform a set of simulations involving idealized disruption of the ocean thermocline by greatly increasing vertical mixing in the upper ocean. We use an Earth System Model (ESM) to evaluate the likely thermal and hydrological response of the atmosphere to this scenario. In our model, increased vertical transport in the upper ocean decreases upward shortwave and longwave radiation at the top-of-the-atmosphere due primarily to loss of clouds and sea-ice over the ocean. This extreme scenario causes an effective radiative forcing of approximate to 15.5-15.9W m(-2), with simulations behaving on multi-decadal time scales as if they are approaching an equilibrium temperature approximate to 8.6-8.8 degrees C higher than controls. Within a century, this produces higher global mean surface temperatures than would have occurred in the absence of increased vertical ocean transport. In our simulations, disruption of the thermocline strongly cools the lower atmosphere over the ocean, resulting in high pressure anomalies. The greater land-sea pressure contrast is found to increase water vapour transport from ocean to land in the lower atmosphere and therefore increase global mean precipitation minus evaporation (P-E) over land; however, many high latitude regions and some low latitude regions experience decreased PE. Any real implementation of ocean pipe technologies would damage the thermal structure of the ocean to a lesser extent than simulated here; nevertheless, our simulations indicate the likely sign and character of unintended atmospheric consequences of such ocean technologies. Prolonged application of ocean pipe technologies, rather than avoiding global warming, could exacerbate long-term warming of the climate system.
引用
收藏
页数:10
相关论文
共 50 条
  • [41] Ocean dynamics, thermocline adjustment, and regulation of tropical SST
    Seager, R
    Murtugudde, R
    JOURNAL OF CLIMATE, 1997, 10 (03) : 521 - 534
  • [42] Southern Ocean intermediate waters in tropical Pacific thermocline
    Pena, L. D.
    Jones, K. M.
    Goldstein, S. L.
    Hemming, S. R.
    Cacho, I.
    GEOCHIMICA ET COSMOCHIMICA ACTA, 2009, 73 (13) : A1010 - A1010
  • [43] PARAMETERIZATION OF THE MIXED LAYER AND SEASONAL THERMOCLINE IN THE OCEAN.
    Belevich, M.Yu.
    Chalikov, D.V.
    1978, (03): : 37 - 43
  • [44] Events of decadal thermocline variations in the South Pacific Ocean
    Jiang Hua
    Wu Dexing
    Wan Xiuquan
    Chinese Journal of Oceanology and Limnology, 2006, 24 (2): : 111 - 117
  • [46] Seasonal thermocline in the China Seas and northwestern Pacific Ocean
    Hao, Jiajia
    Chen, Yongli
    Wang, Fan
    Lin, Pengfei
    JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2012, 117
  • [47] Events of decadal thermocline variations in the South Pacific Ocean
    姜华
    吴德星
    万修全
    Chinese Journal of Oceanology and Limnology, 2006, (02) : 111 - 117
  • [48] A COUPLED ATMOSPHERE OCEAN MODEL IN THE TROPICS WITH DIFFERENT THERMOCLINE PROFILES
    YANG, JY
    OBRIEN, JJ
    JOURNAL OF CLIMATE, 1993, 6 (06) : 1027 - 1040
  • [49] AN INTERCOMPARISON BETWEEN 4 TROPICAL OCEAN MODELS - THERMOCLINE VARIABILITY
    FRANKIGNOUL, C
    FEVRIER, S
    SENNECHAEL, N
    VERBEEK, J
    BRACONNOT, P
    TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 1995, 47 (03) : 351 - 364
  • [50] Holocene variations of thermocline conditions in the eastern tropical Indian Ocean
    Kwiatkowski, Cornelia
    Prange, Matthias
    Varma, Vidya
    Steinke, Stephan
    Hebbeln, Dierk
    Mohtadi, Mahyar
    QUATERNARY SCIENCE REVIEWS, 2015, 114 : 33 - 42