Extended and deep droughts will become commonplace, according to a paper published in PNAS. This scene is from Australia, already affected by deep drought. Photo by Raiden256/flickr.
A new study published in the Proceedings of the National Academy indicates that we are in for a hot 1,000 years from the effects of planet heating caused by our love affair with hydrocarbon fossil fuels.
A key point is that the oceans have been soaking up excess heat and CO2 from the atmosphere and masking the atmospheric warming effects. This also has been causing the oceans to warm up and expand as they soak up heat from the atmosphere.
Because the oceans are so good at storing heat, even if we were to stop burning all fossil fuels tomorrow the effects from the heat-trapping atmospheric greenhouse gases will continue for at least a thousand years as the accumulated heat in the oceans slowly dissipates into the atmosphere.
Further, the paper says there will be significant long-term droughts on a scale with historic "dust bowls," and sea level rise will be significant as warm sea water expands and continental glaciers and ice shelves melt.
None of this is new, really, it's just that the 1,000-year timeline for long-term heating effects from our present activities presents a rather dire picture for those who will inherit this situation from us. And there doesn't appear to be any way out as long as we keep burning coal, oil, and gas at such rapid rates.
PNAS Paper Abstract: "The severity of damaging human-induced climate change depends not only on the magnitude of the change but also on the potential for irreversibility. This paper shows that the climate change that is taking place because of increases in carbon dioxide concentration is largely irreversible for 1,000 years after emissions stop. Following cessation of emissions, removal of atmospheric carbon dioxide decreases radiative forcing, but is largely compensated by slower loss of heat to the ocean, so that atmospheric temperatures do not drop significantly for at least 1,000 years. Among illustrative irreversible impacts that should be expected if atmospheric carbon dioxide concentrations increase from current levels near 385 parts per million by volume (ppmv) to a peak of 450–600 ppmv over the coming century are irreversible dry-season rainfall reductions in several regions comparable to those of the ‘‘dust bowl’’ era and inexorable sea level rise. Thermal expansion of the warming ocean provides a conservative lower limit to irreversible global average sea level rise of at least 0.4 –1.0 m if 21st century CO2 concentrations exceed 600 ppmv and 0.6 –1.9 m for peak CO2 concentrations exceeding 1,000 ppmv. Additional contributions from glaciers and ice sheet contributions to future sea level rise are uncertain but may equal or exceed several meters over the next millennium or longer."
Andrew Revkin, Dot.Earth: The Greenhouse Effect and the Bathtub Effect