the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 21 Apr 2023
ModE-Sim – A medium size AGCM ensemble to study climate variability during the modern era (1420 to 2009)
Eric Samakinwa
Laura Lipfert
Stefan Brönnimann
Abstract. We introduce ModE-Sim, a medium size ensemble of simulations with the atmospheric general circulation model ECHAM6 in its LR version (T63/approx. 1.8° horizontal with 47 vertical levels) that covers the period from 1420 to 2009. With 60 ensemble members between 1420 and 1850 and 36 ensemble members from 1850 to 2009 ModE-Sim consists of 31620 simulated years in total. The dataset forms the input for a data assimilation procedure that combines historical climate informations with additional constraints from a climate model to produce a novel gridded 3-dimensional dataset of the modern era. Additionally, ModE-Sim on its own is also suitable for many other applications as its various subsets can be used as initial condition and boundary condition ensemble to study climate variability. The main intention of this paper is to give a comprehensive description of the experimental setup of ModE-Sim and to provide an evaluation of the two key variables 2m-temperature and precipitation. We demonstrate ModE-Sims ability to represent their mean state, to produce a reasonable response to external forcings and to sample internal variability. At the example of heat waves we show that the ensemble is even capable of capturing extreme events.
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The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
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The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
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Journal article(s) based on this preprint
Ralf Hand et al.
Interactive discussion
Status: closed
-
RC1: 'Comment on egusphere-2023-209', Anonymous Referee #1, 26 May 2023
Summary: The manuscript presents a new dataset of climate simulations spanning approximately five hundred years, generated by the global atmospheric model of the Max-Blank Institute. This ensemble of simulations incorporates variations in external forcing and estimated sea-surface temperature and sea ice cover. The authors assess the realism of these ensembles in reproducing the mean climate, climate variations, and the frequency of heat waves. The manuscript is generally well-written, with clear figures and simulation descriptions. However, there are some concerns with specific sections, such as the one discussing heat waves. Additionally, there are some general comments for the authors to consider in the revised version.
Main points:
1) The manuscript should emphasize that these ensembles cannot capture the internal climate variability originating in the ocean. This is mentioned in the text, but it remains somehow hidden, and at some stages, it may be misleading. This point should be highlighted prominently, even in the abstract and title, as the simulations are driven on observed or reconstructed sea surface temperatures without including the possible internal variability.
2) The section on heat waves needs improvement. The section's title is misleading, as it generally refers to extreme events, not specifically heat waves. The definition of heat waves should be provided in the main text rather than in the caption of Figure 7. The underestimation of heat wave frequency and intensity before 1920 should be acknowledged more explicitly, as it is not a slight discrepancy. The text should avoid suggesting that most heat waves are caused directly by external radiative forcing, as Figure 7 indicates that they are primarily related to mean temperatures. To compare the model's ability to capture extreme events, model biases should be corrected, and heat waves could be defined separately in the reanalysis and model data. This can also be achieved by defining the 95% percentile for reanalysis and for model data separately.
Specific points:
3. The information about data assimilation and a gridded 3-dimensional dataset may not be relevant enough for this manuscript for inclusion in the abstract.
4) The sentence claiming the ensemble's capability to capture extreme events (heat waves) needs careful revision based on the aforementioned points.
5) The phrase "sampling of the supposed true state" is unclear. Clarification is needed, possibly by reformulating the sentence to avoid ambiguity. If by 'true state' the authors mean the mean climate, then this is not a random variable. It is a fixed parameter of the Earth's climate. However, if by 'true state' the authors mean the climatic probability distribution, then the sentence makes sense.
6) Section 2.2 should mention the external forcing used for the simulations upfront rather than referring to it later in the text.
7) In line 108, "set 1430-2" should likely be corrected to "set 1430-3."
8) '' forcing and the ocean boundary conditions can be detected from the subensemble means computed from each 20-member set separately (Fig. 2b & c), indicating that the ensemble size is clearly sufficient to separate forced signals from internal variability'
The distinction between internal atmospheric variability and internal climate variability with oceanic origins is important and should be clarified. The current phrasing might suggest that the ensemble captures all internal climate variability, which is not the case.
Citation: https://doi.org/10.5194/egusphere-2023-209-RC1 -
RC2: 'Comment on egusphere-2023-209', Anonymous Referee #2, 06 Jun 2023
The paper reports on the construction of a single climate model ensemble for the period 1420 to 2009. The ensemble members have different initial conditions but also different boundary conditions (SSTs and sea-ice) and forcings. The climate model is a coarse version of the atmospheric model ECHAM6. The experimental design, including the initial conditions and the forcings, isdescribed in detail. This is followed by a description of the model behavior including the response to volcanic forcings, extremes and heat-waves.
While I value the construction of another large single-model ensemble, and this stands out by including variability related to the uncertainty in the forcings, I cannot recommend that the paper is accepted in its present form. This is a result of the major comments mentioned below.Major comments:
1) The paper seems to be put hastily together. The analysis and results in section 3.4 and 3.5 are very briefly discussed and the methods are basically only described in the figure captions. I can understand that the authors do not wish to present a very deep analysis of heatwaves, but what they choose to show should be adequately described. Figure 3 is only mentioned briefly (l110) and the results are not properly described.
2) Tests of statistical significance are missing throughout the paper. Regions with significant results should be indicated in the figures.
3) I have several comments to the construction of the additional SSTs in Section 2.2.3. First of all the construction is not linear as claimed. A linear model would look like SST_i = 1/3(SST_j + SST_k + SST_l).
Furthermore, I think x and t should be dropped from the formula and it should just be mentioned in the text that the construction is applied simultaneously to grid-points and time.
More importantly, the authors should also be aware that their method generates SSTs that donot have a Gaussian distribution. The distribution of a ratio like SST_j/SST_k has heavy tails. It is difficult to see how big this problem is here, but it will also depend of the units you use for temperature (I hope it is Kelvin).
Minor comments:
Abstract: The data assimilation procedure is mentioned but it is not clear if this is for the future or if it is included in the present paper. Perhaps the abstract could be more informative on the results of the paper.
l16: This refer to single-models ensembles only. Multi-model ensembles also include differences in physics. I think the difference between the two types of ensembles should be stated directly here.
l22: This sentence is not clear. .. was done by comparison with the statistics .. Comparison with what?
l43 A time-slice is mentioned but which time-slice.
l46: Perhaps define modern era in the text.
l57: 'last': as in latest or final?
l103: Is EVA defined anywhere?
l108: 1430-2 --> 1430-3 ?
l168: Perhaps the warming over northern Eurasia is connected to a positive NAO. A positive NAO is reported in observational studies the winter after the eruptions (see, e.g., Christiansen 10.1175/2007JCLI1657.1).
Section 3.3: How does the model reproduce the temporal characteristic of the ENSO? The responses in Fig. 5 seem very spatial extended. The statistical significance is important here.
Figure 2: It is hard to see the shading in panels b and c.
Figure 4: The statistical significance describing where this signal is different from zero should be indicated. The caption says 'ensemble mean': I guess this is the mean of the volcanic signal over the ensemble members and not the signal in the ensemble mean temperature. This should be explained better.
Line 210 and Fig. 6: The description here is so brief that it is almost impossible to understand.
Section 3.5: Again, I find this much too brief to be of any value.Citation: https://doi.org/10.5194/egusphere-2023-209-RC2 - AC1: 'Comment on egusphere-2023-209', Ralf Hand, 27 Jul 2023
Interactive discussion
Status: closed
-
RC1: 'Comment on egusphere-2023-209', Anonymous Referee #1, 26 May 2023
Summary: The manuscript presents a new dataset of climate simulations spanning approximately five hundred years, generated by the global atmospheric model of the Max-Blank Institute. This ensemble of simulations incorporates variations in external forcing and estimated sea-surface temperature and sea ice cover. The authors assess the realism of these ensembles in reproducing the mean climate, climate variations, and the frequency of heat waves. The manuscript is generally well-written, with clear figures and simulation descriptions. However, there are some concerns with specific sections, such as the one discussing heat waves. Additionally, there are some general comments for the authors to consider in the revised version.
Main points:
1) The manuscript should emphasize that these ensembles cannot capture the internal climate variability originating in the ocean. This is mentioned in the text, but it remains somehow hidden, and at some stages, it may be misleading. This point should be highlighted prominently, even in the abstract and title, as the simulations are driven on observed or reconstructed sea surface temperatures without including the possible internal variability.
2) The section on heat waves needs improvement. The section's title is misleading, as it generally refers to extreme events, not specifically heat waves. The definition of heat waves should be provided in the main text rather than in the caption of Figure 7. The underestimation of heat wave frequency and intensity before 1920 should be acknowledged more explicitly, as it is not a slight discrepancy. The text should avoid suggesting that most heat waves are caused directly by external radiative forcing, as Figure 7 indicates that they are primarily related to mean temperatures. To compare the model's ability to capture extreme events, model biases should be corrected, and heat waves could be defined separately in the reanalysis and model data. This can also be achieved by defining the 95% percentile for reanalysis and for model data separately.
Specific points:
3. The information about data assimilation and a gridded 3-dimensional dataset may not be relevant enough for this manuscript for inclusion in the abstract.
4) The sentence claiming the ensemble's capability to capture extreme events (heat waves) needs careful revision based on the aforementioned points.
5) The phrase "sampling of the supposed true state" is unclear. Clarification is needed, possibly by reformulating the sentence to avoid ambiguity. If by 'true state' the authors mean the mean climate, then this is not a random variable. It is a fixed parameter of the Earth's climate. However, if by 'true state' the authors mean the climatic probability distribution, then the sentence makes sense.
6) Section 2.2 should mention the external forcing used for the simulations upfront rather than referring to it later in the text.
7) In line 108, "set 1430-2" should likely be corrected to "set 1430-3."
8) '' forcing and the ocean boundary conditions can be detected from the subensemble means computed from each 20-member set separately (Fig. 2b & c), indicating that the ensemble size is clearly sufficient to separate forced signals from internal variability'
The distinction between internal atmospheric variability and internal climate variability with oceanic origins is important and should be clarified. The current phrasing might suggest that the ensemble captures all internal climate variability, which is not the case.
Citation: https://doi.org/10.5194/egusphere-2023-209-RC1 -
RC2: 'Comment on egusphere-2023-209', Anonymous Referee #2, 06 Jun 2023
The paper reports on the construction of a single climate model ensemble for the period 1420 to 2009. The ensemble members have different initial conditions but also different boundary conditions (SSTs and sea-ice) and forcings. The climate model is a coarse version of the atmospheric model ECHAM6. The experimental design, including the initial conditions and the forcings, isdescribed in detail. This is followed by a description of the model behavior including the response to volcanic forcings, extremes and heat-waves.
While I value the construction of another large single-model ensemble, and this stands out by including variability related to the uncertainty in the forcings, I cannot recommend that the paper is accepted in its present form. This is a result of the major comments mentioned below.Major comments:
1) The paper seems to be put hastily together. The analysis and results in section 3.4 and 3.5 are very briefly discussed and the methods are basically only described in the figure captions. I can understand that the authors do not wish to present a very deep analysis of heatwaves, but what they choose to show should be adequately described. Figure 3 is only mentioned briefly (l110) and the results are not properly described.
2) Tests of statistical significance are missing throughout the paper. Regions with significant results should be indicated in the figures.
3) I have several comments to the construction of the additional SSTs in Section 2.2.3. First of all the construction is not linear as claimed. A linear model would look like SST_i = 1/3(SST_j + SST_k + SST_l).
Furthermore, I think x and t should be dropped from the formula and it should just be mentioned in the text that the construction is applied simultaneously to grid-points and time.
More importantly, the authors should also be aware that their method generates SSTs that donot have a Gaussian distribution. The distribution of a ratio like SST_j/SST_k has heavy tails. It is difficult to see how big this problem is here, but it will also depend of the units you use for temperature (I hope it is Kelvin).
Minor comments:
Abstract: The data assimilation procedure is mentioned but it is not clear if this is for the future or if it is included in the present paper. Perhaps the abstract could be more informative on the results of the paper.
l16: This refer to single-models ensembles only. Multi-model ensembles also include differences in physics. I think the difference between the two types of ensembles should be stated directly here.
l22: This sentence is not clear. .. was done by comparison with the statistics .. Comparison with what?
l43 A time-slice is mentioned but which time-slice.
l46: Perhaps define modern era in the text.
l57: 'last': as in latest or final?
l103: Is EVA defined anywhere?
l108: 1430-2 --> 1430-3 ?
l168: Perhaps the warming over northern Eurasia is connected to a positive NAO. A positive NAO is reported in observational studies the winter after the eruptions (see, e.g., Christiansen 10.1175/2007JCLI1657.1).
Section 3.3: How does the model reproduce the temporal characteristic of the ENSO? The responses in Fig. 5 seem very spatial extended. The statistical significance is important here.
Figure 2: It is hard to see the shading in panels b and c.
Figure 4: The statistical significance describing where this signal is different from zero should be indicated. The caption says 'ensemble mean': I guess this is the mean of the volcanic signal over the ensemble members and not the signal in the ensemble mean temperature. This should be explained better.
Line 210 and Fig. 6: The description here is so brief that it is almost impossible to understand.
Section 3.5: Again, I find this much too brief to be of any value.Citation: https://doi.org/10.5194/egusphere-2023-209-RC2 - AC1: 'Comment on egusphere-2023-209', Ralf Hand, 27 Jul 2023
Peer review completion
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Ralf Hand et al.
Ralf Hand et al.
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The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
- Preprint
(5935 KB) - Metadata XML
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Supplement
(4400 KB) - BibTeX
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- Final revised paper