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H2 effects on CH4 lifetime #758
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…rs in the gcam coupling
…ead in from teh ini file
Differences in Hector outputsHello, this is The current pull request's outputs do not differ from 3.1.1 (d931a00). |
Some specific questions for @ssmithClimate & @bpbond
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Differences in Hector outputsHello, this is The current pull request's outputs do not differ from 3.1.1 (d931a00). |
Differences in Hector outputsHello, this is The current pull request's outputs do not differ from 3.1.1 (d931a00). |
Unless we reasonably expect that users will want to run sensitivity tests or otherwise manipulate these parameters, I'd vote to start with NOT exposing them via R or the INI file. Name:
When you say "undefined", you mean they have no units? That's OK, but if you know the associated units, we might as well include them for clarity. |
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Overall looks good! THANK YOU @kdorheim
inst/input/hector_ssp119.ini
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@@ -138,6 +138,7 @@ CNOX=0.0042 ; coefficent for NOX | |||
CCO=-0.000105 ; coefficent for CO | |||
CNMVOC=-0.000315 ; coefficent for NMVOC (non methane VOC) | |||
CCH4=-0.32 ; coefficent for CH4 | |||
CH2=-0.00044625 ; coefficent for H2 |
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Same spelling note; also, is there a reference/source for this value? If so please note it.
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Was there some derivation needed for this, or was this coefficient in the right format from the original source? (And how similar were the coefficients for other emissions to the ones we are using now?)
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Okay there was a derivation that was needed for this parameter, which will be described in detail in the manuscript associated with this work although that is a TBD, so I have included a TODO-H2 tag which is linked to the H2 project as a reminder to address this issue before merging into main or anything.
@ssmithClimate Could you elaborate on this a bit more? (And how similar were the coefficients for other emissions to the ones we are using now?) I am not sure if I understand what you are asking here. It is also unclear where the original coefficients came from @ssmithClimate do you know the source of those?
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Sorry for the delay. The coefficients in hector now ultimately derive from this paper:
Wigley, T.M.L., Steven J. Smith, and M.J. Prather (2002) Radiative Forcing due to Reactive Gas Emissions. Journal of Climate 15(18), pp. 2690–2696
Although the hector paper quotes the source as :
Tanaka, K., Kriegler, E., Bruckner, T., Hooss, C., Knorr, W., and Raddatz, T.: Aggregated Carbon Cycle, Atmospheric Chemistry, and Climate Model (ACC2) – description of the forward and inverse models, 1–188, Max Planck Institute for Meteorology, Hamburg, Germany, 188, 2007.
(which is a more indirect reference)
So my question was - is the overall chemistry representation of the source we're drawing the H2 coefficients from is generally consistent with the chemistry representation used now in Hector. If not it's something to flag (e.g., means we ultimately might need to update more than H2) since the two things we're merging together are not entirely consistent with each other. (Given uncertainty its likely fine, but we would want to flag this at least.)
So the way I thought to evaluate that was to look if the relative magnitude of any common coefficients for the non-H2 components of the equations that were used in the H2 work we're using now and the original equation we use now in Hector were similar. For example is the ratio of the impact of NOx to impact of CH4 or NOx to CO in the original hector (e.g. Wigley et al, Tanaka et al) are similar to what's in the H2 papers we are citing (to the extent they contain these other effects).
For example, in hector we have something like this for the CH4 OH lifetime (Hartin et al. 2015):
ln(OH)t = −0.32(ln[CH4 ]t − ln[CH4 ]t 0 ) + 0.0042(E(NOx)t ) − (E(NOx)t0) − 0.000105(E(CO)t ) − (E(CO)t0) − 0.00315(E(VOC)t ) − (E(VOC)t0)
So the impact of NOx vs CO is: 0.0042 / 0.000105 = 40 times (on an emissions basis in this case). Or we could look at the relative impact of NOx to CH4 in this equation if that's what's common between what's in hector now and what is represented in the equations from the paper's we are drawing from for the new H2 components.
To do this we need to have both sets of equations cast into an equivalent form.
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@kdorheim comments here!
@kdorheim - just a couple comments, this is great to see! |
Okay I can remove the coeff from the R bindings but all of the coefficients have been defined in the ini file I think since V1 |
I'm confused; this may be easier to talk through in person. Anyway, |
Differences in Hector outputsHello, this is The current pull request's outputs do not differ from 3.1.1 (d931a00). |
NOTE: this PR is targeting the dev-h2 branch
This branch implements the H2 effects on CH4, it will close #749. We have added equation (5) into Hector to account for how$H_2$ interacts with OH, decreasing the amount of OH that can interact with $[CH_4]$ . We derived the value for the $c_{H_2}$ from Bertagni et al. 2022.
Since we don't have$H_2$ emissions for the historical or future periods, we shouldn't see any changes in Hector results (Leeyabot or the old new tests). In order to get a feel for how this development affects Hector results I've included some results from emission impulse runs.
This first figure shows results from three Hector runs, a constant emission-driven run, and then two impulse runs varying in magnitude. It is intended to show how this model development cascades throughout the model. The pulse of$H_2$ emissions causes $\tau_{OH}$ (methane's lifetime with respect to OH) to change, which causes $[CH_4]$ to change, which is what we were expecting. Since in Hector the trop. $O_3$ burden and strat. $H_2O$ vapor radiative forcing computations are proportional to $[CH_4]$ the $H_2$ emissions pulse affects these variables as well.
This second figure demonstrates the sensitivity of impulse response to our new parameter$c_{H_2}$ . As we would hope, increasing and decreasing this parameter changes the system response.
In this third figure, we compare the RF response from unit emission of$CO_2$ and $H_2$ 100 years after the emissions impulse, which can be used to calculate the GWP100. Hector's GWP100 for H2 ~ 5.17 is consistent with the Sand et al. results included in Supplementary Table 6. Sand et al. found the GWP100 of hydrogen due to methane ranges from 4.9 to 5.7 with a model mean of 5.1, which is not too far off what we are getting from Hector at the moment!
References
Bertagni, M. B., Pacala, S. W., Paulot, F., & Porporato, A. (2022). Risk of the hydrogen economy for atmospheric methane. Nature Communications, 13(1), 7706.
Sand, M., Skeie, R. B., Sandstad, M., Krishnan, S., Myhre, G., Bryant, H., Derwent, R., Hauglustaine, D., Paulot, F., Prather, M., & Stevenson, D. (2023). A multi-model assessment of the Global Warming Potential of hydrogen. Communications Earth & Environment, 4(1), 1–12.
Materials Used
PR-758.zip