BEYOND 2 DEGREES CELSIUS: Implications of NASA/GISS updates for the Earth energy balance, global temperatures, ice melt and sea level rise
Dr Andrew Glikson (Earth and Paleoclimate Science, Australian National University)
30 May 2011
The Earth energy balance—namely the difference between energy/heat absorbed by the Earth from solar radiation and the energy/heat emitted back to space—estimated at +3.1 Watt/m², equivalent to a +2.3 °C (based on climate sensitivity of 3 °C per doubling of CO2) (Hansen et al., 2011 [1]), is currently in
part mitigated by the cooling effect of albedo-enhancing sulphur aerosols (~ -1.6 Watt/m² = ~ -1.2 °C) emitted from fossil fuels and industry, which effectively act as a global geo-engineering process (Figure 1).
Had it not been for this short-lived (few years long) cooling effect, the internationally agreed maximum
temperature target of < 2 °C would be transcended.
According to the IPCC AR4 (2007) [2] mean global land/ocean temperature since 1880 has risen by about +0.8 °C, which translates to more than +4 °C rise in the polar region of northern Canada, Greenland and Siberia [3] (Figure 2), triggering feedback-amplified ice melting accelerating between 2002 and 2010 [4] (Figure 3) and related sea level rise at a rate of 3.0 ± 0.4 mm/year between 1993-2010 (Figure 4A). Melting of Arctic ice leading to increased evaporation can result in the advance of cold fronts into the north Atlantic (Figure 4B). The measured global warming of +0.8 °C is lagging behind the +1.1 °C rise required by the energy imbalance (Figure 1B), a lag attributable to the buffering effect of the oceans. The temperature rise lag period has been estimated as 35 years [5].
Prior to the Copenhagen conference in 2009 the European Union obtained the agreement of relevant partners—including China, India, Russia, and the United States—to commit to an upper 2 °C ceiling on further rise in mean global temperature in order to avoid the risk of dangerous climate change [6]. However,
a rise beyond 2 °C may lead to tipping points in the atmosphere/ocean system [10]. As stated by the NASA/GISS climate science group [11], “Decreasing CO2 was the main cause of a cooling trend that began 50 million years ago, large scale glaciation occurring when CO2 fell to 425 ± 75 ppm, a level that will be exceeded within decades, barring prompt policy changes. If humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, paleoclimate evidence and ongoing climate change suggest that CO2 will need to be reduced from its current 385 ppm to at most 350 ppm. The largest uncertainty in the target arises from possible changes of non-CO2 forcings. An initial 350 ppm CO2 target may be achievable by phasing out coal use except where CO2 is captured and adopting agricultural and forestry practices that sequester carbon. If the present overshoot of this target CO2 is not brief, there is a possibility of seeding irreversible catastrophic effects.”
With current CO2 levels rising to ~28,000 million tons by 2010 (Figure 5) at rates fluctuating around ~2 ppm/year, reaching a level of 393.18 ppm at Mauna Loa in April 2011 [7] (Figure 6), with a total CO2-e (which includes CO2 + the equivalent effect of methane) of > 460 ppm [8], the NASA/GISS study [1] implies global warming committed to reach 2.3 °C once the aerosol effect dissipates [12] (Figure 1). This effective though unintended geoengineering measure, acting as a transient shield from a near-doubling of global warming, further lowers ocean pH on top of CO2 sequestration.
Had the proposed Australian reduction of 5% in the rate of carbon emissions by 2020 relative to 2000 [9] been a figure adopted world-side, global emissions would be reduced from ~24,000 million tons/year to 22,500 million tons/year, hardly causing a dent in the current trajectory above 393 ppm CO2 toward levels at which the polar ice sheets are further destabilized (Figure 3).
It is not clear whether deep reduction in carbon emissions will be sufficient to stem the amplifying feedbacks associated with greenhouse gas warming and ice/melt water interactions. Barring an indefinite maintenance of sulphur aerosol emissions, deep emission cuts need to be accompanied by atmospheric CO2 draw-down by means of fast-track tree planting, application of biochar methods and chemical CO2 sequestration. As shown by the intensifying spate of extreme weather events around the globe (Figure 7), the alternative bears no
contemplation.
Figures (well worth having a look|) and references here: http://www.countercurrents.org/glikson290511.pdf
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