Millennial timescale carbon cycle and climate change in an efficient Earth system model

نویسندگان

  • T. M. Lenton
  • M. S. Williamson
  • N. R. Edwards
  • R. Marsh
  • A. R. Price
  • A. J. Ridgwell
  • J. G. Shepherd
چکیده

A new Earth system model, GENIE-1, is presented which comprises a 3-D frictional geostrophic ocean, phosphate-restoring marine biogeochemistry, dynamic and thermodynamic sea-ice, land surface physics and carbon cycling, and a seasonal 2-D energy-moisture balance atmosphere. Three sets of model climate parameters are used to explore the robustness of the results and for traceability to earlier work. The model versions have climate sensitivity of 2.8-3.3◦C and predict atmospheric CO2 close to present observations. Six idealized total fossil fuel CO2 emissions scenarios, are used to explore a range of 1,100-15,000 GtC total emissions and the effect of rate of emissions. Atmospheric CO2 approaches equilibrium in year 3000 at 420-6000 ppmv, giving 1.5-10.5◦C global warming. The ocean is a robust carbon sink of up to 9 GtC yr−1. Under ‘business as usual’, the land becomes a carbon source around 2100 which peaks at up to 2 GtC yr−1. Soil carbon is lost globally, boreal vegetation generally increases, whilst under extreme forcing, dieback of some tropical and sub-tropical vegetation occurs. Average ocean surface pH drops by up to 1.15 units. A Greenland ice sheet melt threshold of 2.6◦C local warming is just avoided if total emissions are limited to 1,100 GtC, whilst 15,000 GtC emissions cause complete Greenland melt by year 3000, contributing 7m to sea level rise. Total sea-level rise, including thermal expansion, is 0.4-10m in year 3000 and ongoing. The Atlantic meridional overturning circulation shuts down in 2 out of 3 model versions, but only under extreme emissions including exotic fossil fuel resources. ∗Tyndall Centre, UK and School of Environmental Sciences, University of East Anglia, Norwich, UK. E-mail: [email protected] Tel: +44-1603-591414 Fax: +44-1603-507719 †Earth Sciences, Open University, Milton Keynes, UK ‡Tyndall Centre, UK and National Oceanography Centre, Southampton, UK §Southampton e-Science Centre, University of Southampton, Southampton, UK ¶Department of Earth and Ocean Sciences, University of British Columbia, Vancouver, Canada ‖www.genie.ac.uk/people

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

The effects of changing solar activity on climate: contributions from palaeoclimatological studies

Natural climate change currently acts in concert with human-induced changes in the climate system. To disentangle the natural variability in the climate system and the human-induced effects on the global climate, a critical analysis of climate change in the past may offer a better understanding of the processes that drive the global climate system. In this review paper, we present palaeoclimato...

متن کامل

Climate sensitivity to the carbon cycle modulated by past and future changes in ocean chemistry

The carbon cycle has a central role in climate change. For example, during glacial–interglacial cycles, atmospheric carbon dioxide has altered radiative forcing and amplified temperature changes. However, it is unclear how sensitive the climate system has been to changes in carbon cycling in previous geological periods, or how this sensitivity may evolve in the future, following massive anthrop...

متن کامل

Bipolar correlation of volcanism with millennial climate change.

Analyzing data from our optical dust logger, we find that volcanic ash layers from the Siple Dome (Antarctica) borehole are simultaneous (with >99% rejection of the null hypothesis) with the onset of millennium-timescale cooling recorded at Greenland Ice Sheet Project 2 (GISP2; Greenland). These data are the best evidence yet for a causal connection between volcanism and millennial climate chan...

متن کامل

The millennial atmospheric lifetime of anthropogenic CO2

The notion is pervasive in the climate science community and in the public at large that the climate impacts of fossil fuel CO2 release will only persist for a few centuries. This conclusion has no basis in theory or models of the atmosphere/ocean carbon cycle, which we review here. The largest fraction of the CO2 recovery will take place on time scales of centuries, as CO2 invades the ocean, b...

متن کامل

Biosphere feedbacks and climate change

POLICY ACTION ON CLIMATE CHANGE IS INFORMED BY CLIMATE MODEL projections as described most recently in the Fifth Assessment Report (AR5) of the Intergovernmental Panel on Climate Change (IPCC). The models used are general circulation models (GCMs), which numerically represent the physical climate system in three dimensions, including the hydrological cycle. These are complemented by recently de...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

عنوان ژورنال:

دوره   شماره 

صفحات  -

تاریخ انتشار 2005