- #36
Catamount
- 4
- 0
It's true that if the BAU scenario did outpace what really happened for carbon dioxide, it wasn't by much. However that scenario had enormously higher methane emissions growth than actually occurred, projecting a near linear growth of emissions where the real world saw what appears to be emissions that went from static yearly inputs to drastic decrease, followed by resumed emissions at only a very modest level compared to the 90s. Far from growing from 350ish MtC/yr and blowing past 400, 500, and more, emissions appear to have tanked by 2000, and only modestly resume in the 2010s if concentration numbers are any indication.
http://www.esrl.noaa.gov/gmd/aggi/aggi.fig2.png
Strangely, I'm having a hard time finding emissions numbers past the late 90s, but nevertheless, concentration change has stalled out pretty strongly, especially compared to the ever-accelerating concentrations rise in FAR's BAU scenario. If emissions had increased the concentration would have started changing faster, not stalled out (obviously).Of course, the more important point is going to be that no matter what, these scenarios are going to be overestimations of net forcings, because they're not going to include the hugely negative trends in the ENSO forcing or recent aerosol hikes. Most of DH's points of criticism are very cogent, and that's one of the biggest. FAR didn't use what we'd consider a full and proper GCM. They just used a simple radiation balance model with a little bit of ocean behavior thrown in which appears to have just been there to moderate the rate of change. That's not even going to account for something like ENSO, let alone represent a correct prediction of the trends of such a forcing that would be necessary to build a proper scenario to test.I believe that may also represent a big criticism of Moncton et al taht DH didn't seem to bring up, but I'm just a layman so I'd be happily corrected there: Moncton et al. appear to basically get their past 20ish-years period by modelling all of climate over that recent period as a response to CO2, deriving the level of climatic response to CO2 by simply subtracting the other major forcings in play outlined by the IPCC and just assuming that anything that remains is CO2->temperature response, and then just plotting that sort of sensitivity of temperature to CO2 over time with the assumption that it's going to explain all behavior over the period they're using for comparison of their model to FAR. Is that going to include the influence of any short-term climatic behavior like ENSO? It doesn't seem so to me. So if that bottoms out, and you get a negative forcing that their simple model doesn't account for, it's going to manifest as reduced sensitivity, and we did have bottomed out short-term natural forcings and increased aerosol production from Asia, and oh hey, look what happened! They got really low sensitivity! Is my admitted lack of expertise here causing me to miss some hidden genius to their methods, or is it really that bad?More to the point, are the models, the modern models, actually overestimating warming? Gavin Schmidt and his co-authors in a recent little piece in Nature Geoscience don't think so. When they took their best shot at including the most up-to-date estimates of the forcings, different than what CMIP5 models are using, most of the disagreement between the temperature and the models disappeared
http://www.blc.arizona.edu/courses/schaffer/182h/Climate/Reconciling Warming Trends.pdf
http://www.esrl.noaa.gov/gmd/aggi/aggi.fig2.png
Strangely, I'm having a hard time finding emissions numbers past the late 90s, but nevertheless, concentration change has stalled out pretty strongly, especially compared to the ever-accelerating concentrations rise in FAR's BAU scenario. If emissions had increased the concentration would have started changing faster, not stalled out (obviously).Of course, the more important point is going to be that no matter what, these scenarios are going to be overestimations of net forcings, because they're not going to include the hugely negative trends in the ENSO forcing or recent aerosol hikes. Most of DH's points of criticism are very cogent, and that's one of the biggest. FAR didn't use what we'd consider a full and proper GCM. They just used a simple radiation balance model with a little bit of ocean behavior thrown in which appears to have just been there to moderate the rate of change. That's not even going to account for something like ENSO, let alone represent a correct prediction of the trends of such a forcing that would be necessary to build a proper scenario to test.I believe that may also represent a big criticism of Moncton et al taht DH didn't seem to bring up, but I'm just a layman so I'd be happily corrected there: Moncton et al. appear to basically get their past 20ish-years period by modelling all of climate over that recent period as a response to CO2, deriving the level of climatic response to CO2 by simply subtracting the other major forcings in play outlined by the IPCC and just assuming that anything that remains is CO2->temperature response, and then just plotting that sort of sensitivity of temperature to CO2 over time with the assumption that it's going to explain all behavior over the period they're using for comparison of their model to FAR. Is that going to include the influence of any short-term climatic behavior like ENSO? It doesn't seem so to me. So if that bottoms out, and you get a negative forcing that their simple model doesn't account for, it's going to manifest as reduced sensitivity, and we did have bottomed out short-term natural forcings and increased aerosol production from Asia, and oh hey, look what happened! They got really low sensitivity! Is my admitted lack of expertise here causing me to miss some hidden genius to their methods, or is it really that bad?More to the point, are the models, the modern models, actually overestimating warming? Gavin Schmidt and his co-authors in a recent little piece in Nature Geoscience don't think so. When they took their best shot at including the most up-to-date estimates of the forcings, different than what CMIP5 models are using, most of the disagreement between the temperature and the models disappeared
http://www.blc.arizona.edu/courses/schaffer/182h/Climate/Reconciling Warming Trends.pdf
Last edited: