Simulated changes in vegetation distribution, land carbon storage, and atmospheric CO2 in response to a collapse of the North Atlantic thermohaline circulation |
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| Authors: | Peter Köhler Fortunat Joos Stefan Gerber Reto Knutti |
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| Institution: | (1) Alfred Wegener Institute for Polar and Marine Research, PO Box 120161, 27515 Bremerhaven, Germany;(2) Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstr 5, 3012 Bern, Switzerland;(3) Princeton University, Princeton Forrestal Campus 201, Forrestal Road, PO Box 308, Princeton, NJ 08542-0308, USA;(4) National Center for Atmospheric Research, PO Box 3000, Boulder, CO 80307-3000, USA |
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| Abstract: | It is investigated how abrupt changes in the North Atlantic (NA) thermohaline circulation (THC) affect the terrestrial carbon
cycle. The Lund–Potsdam–Jena Dynamic Global Vegetation Model is forced with climate perturbations from glacial freshwater
experiments with the ECBILT-CLIO ocean–atmosphere–sea ice model. A reorganisation of the marine carbon cycle is not addressed.
Modelled NA THC collapses and recovers after about a millennium in response to prescribed freshwater forcing. The initial
cooling of several Kelvin over Eurasia causes a reduction of extant boreal and temperate forests and a decrease in carbon
storage in high northern latitudes, whereas improved growing conditions and slower soil decomposition rates lead to enhanced
storage in mid-latitudes. The magnitude and evolution of global terrestrial carbon storage in response to abrupt THC changes
depends sensitively on the initial climate conditions. These were varied using results from time slice simulations with the
Hadley Centre model HadSM3 for different periods over the past 21 kyr. Changes in terrestrial storage vary between −67 and
+50 PgC for the range of experiments with different initial conditions. Simulated peak-to-peak differences in atmospheric
CO2 are 6 and 13 ppmv for glacial and late Holocene conditions. Simulated changes in δ13C are between 0.15 and 0.25‰. These simulated carbon storage anomalies during a NA THC collapse depend on their magnitude
on the CO2 fertilisation feedback mechanism. The CO2 changes simulated for glacial conditions are compatible with available evidence from marine studies and the ice core CO2 record. The latter shows multi-millennial CO2 variations of up to 20 ppmv broadly in parallel with the Antarctic warm events A1 to A4 in the South and cooling in the North. |
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