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Comments received July 7 – August 12, 2004 ReviewersWilliam Fang/Eric Holdsworth Wolf Grossmann Haroon Kheshgi William O’Keefe Charles F. Keller Michael MacCracken Jim Meyer Asmunn Moene Ellis E. Remsberg John Stone General CommentsWilliam Fang/Eric HoldsworthEEI made rather extensive comments on the general guidelines, which we understand from the instructions accompanying the Federal Register notice (69 Fed. Reg. 42043) “are being revised,” taking into consideration the comments received” from EEI and others and notes that this prospectus does not reflect any of those comments, such as our comments on “selection of authors” and on the issues of “confidence levels” and probabilities. However, we also understand that when a “final version of the guidelines” is available, this prospectus “will be revised if necessary to conform fully to the final version of the guidelines.” While that is certainly good, it is difficult to understand at this juncture how and to what extent those revisions will change our understanding of this Prospectus, particularly the phase 1 and 2 schedule, which is already too tight and inconsistent with the Strategic Plan, which affords up to “2 years” for completion. This schedule affords a little more than one year for completion, with a large segment of that time (Jan. 05-Nov. 05) devoted to review and clearance. While it is important to get the work on the products underway, it is not in the public interest to rush them, particularly in light of the unfinished nature of the guidelines. According to Phase 1 of the “Draft Prospectus,” it is to be approved this month. Yet it is unclear when the guidelines will be revised and finalized. No date is given in the instructions. Most importantly, the Instructions do not indicate how and when the final version of the Prospectus is to be made available to the public with these revisions. Wolf GrossmannThis is not my area of expertise. I feel quite comfortable at linking climate and society, in particular societal and economic change, and I have written papers and that subject, build dynamic integrated models on it and feel quite comfortable with this subject area as the workshop from Dec. 2002 came out with the conclusion that this is a subject area of outstanding importance for the future of getting things implemented. So, I hope I will hear initiatives also from that subject area and are very much looking forward to that! Charles KellerFirst General: Overall publication setup. Perhaps there's no other way to change it, but this format sounds at least somewhat like a way to minimize the UAH people's (John Christy and Roy Spencer) results of small warming trend. The key element in this format seems to be to establish that uncertainties in observational measurements are larger than UAH has claimed in print. Once that is established, the small warming result's agreement with radiosonde data can be called into question. If true, it this really the right way to go? Might not a better approach be to attempt to show by an independent evaluation just how well UAH and radiosonde results support each other as compared with RSS results? Haroon KheshgiFirst General: Using atmospheric records of temperature to improve our understanding of climate change presents an important component of climate change research. In particular, understanding what is the deficiency in our understanding that is the cause of the apparent discrepancy between tropospheric and surface temperature records is a key question to be resolved. The IPCC TAR SPM noted that "these differences are not fully resolved." While this prospectus begins to address this topic, it has a number of weaknesses that will prevent it from fully assessing the topic of the apparent discrepancies. These weaknesses are elaborated in the following comments:
Michael MacCracken
Jim Meyer
Asmunn MoeneGlobal mean temperature changes are unpredictable
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The figure illustrates the global mean temperature changes from 1979 measured at the surface and in the lower troposphere by satellite (NASA). To compare the trends directly they are referred to a common zero point. |
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The figure illustrates the global mean temperature changes from 1979 measured at the surface and in the lower troposphere by satellite (NASA). To compare the trends directly they are referred to a common zero point. The prognoses of the international panel of climate change, IPCC, show a temperature increase of 1,4 - 4,5°C in 100 years caused by a doubling of the CO2 content in the atmosphere. In the figure a trend of 0,3° pr. decade is given. There is no significant relationship between the IPCC predicted trend and the two other curveswhich are generated by random changes. The random updating is of fundamental importance. Such systems are called autoregressive and they are nondeterministic i.e. they are unpredcitable. Further the curves do not quite fulfil the requirement necessary in order to be an independent Gaussian process, which one must assume if one is to use a model for statistical forecasting. The figure demonstrates another important fact: An increase of the CO2 - content in the atmosphere should create a greater warming trend in the lower troposphere i.e .a greenhouse effect. It is evident that this is actually not he case. The warming trend is greater at the surface than in the lower troposphere. According to the models introduced by IPCC the position of the two curves should be interchanged .The tropospheric warming trend is supposed to be 1,5 to 2,0 times greater than at the surface if the greenhouse gases are the cause. It also appears from the last report of IPCC, (page 106), that the largest difference between surface and satellite measurements is found over the tropical and subtropical oceans where the most important accumulation of solar heat takes place on the earth. The dominant warming trend at the surface therefore has to be caused by the world oceans covering above 70% of the surface of the earth. William O’KeefeThe CCSP has chosen an appropriate set of technical questions to address in its first Synthesis and Assessment Product. The authors chosen to address these questions are well qualified and represent the spectrum of scientific opinion on this topic. The credibility of this synthesis and assessment product would be greatly enhanced if an eminent scientist not directly involved in the issues being addressed was chosen as convening lead author for the summary question. There is no question that Dr. Wigley is a highly qualified climate change scientist, and we do not question his scientific integrity. However he, and any other similarly qualified climate change scientist, will have formed views on the issues under discussion in this product long before drafting of the summary begins. It would be very difficult for any scientist deeply involved in the issues to take an entirely fresh view of the information compiled in the synthesis and assessment. The critical goal of CCSP synthesis and assessment products is to analyze the available information on climate change science issues and present it in a fashion that responds to the questions raised by policymakers. A fresh, neutral view of the underlying information is critical, and can provide insights that may have escaped those who directly involved in the collection and analysis of the data. An example of the value of a fresh view is the role played by Freeman Dyson in the investigation of the Shuttle Challenger disaster. An eminent scientist with a background in analyzing and explaining experimental data should be chosen as the convening lead author for the summary question. Dr. Wigley and the convening lead authors of the six underlying questions should compose the writing team for the summary question. They bring the expertise needed to ensure that all information and points-of-view are considered in responding to the summary question. Some might argue that the CCSP review process ensures that fresh points-of-view are included in the synthesis and assessment product. While the review process should ensure that all available information is considered, it is not an interactive process. Reviewers submit their comments, which are considered by the author teams, but it is a static, one-off, process. The dynamic interaction that leads to the development of new analyses is missing. Having a distinguished scientist from outside the climate change science community challenging the conventional wisdom on surface and atmospheric temperature data and modeling in an interactive debate with the scientists most responsible for generating the underlying information offers an opportunity to generate new insights and approaches that should not be missed. Ellis RemsbergSeveral months ago an important paper appeared in the May 6, 2004 issue of the journal Nature (Fu, Johanson, Warren, and Seidel, pp. 55-58). In my opinion their study largely explains the relatively long-standing discrepancy about temperature trends in the lower troposphere as obtained from the MSU satellite instruments versus those from surface-based temperature records. My expertise in the area of atmospheric remote sensing by atmospheric emission techniques from satellite platforms leads me to see how it is easily possible to have measurements from a vertical weighting function that peaks in the lower stratosphere to be "contaminating" the record of trends from a more primary vertical weighting function that is centered in the lower troposphere. In my opinion the findings of these authors should be hailed as definitive for the settling of this so-called "controversy", and the climate research community should be moving on to other issues, such as how to ensure that a good quality temperature monitoring record be maintained with future global, satellite observing systems. John StoneThis is excellent. The choice of questions should probe our physical understanding of the system we are observing, the detection of changes from natural variability, and the attribution based on our physical understanding. The choice of the author team is similarly excellent. You have been able to engage some first class scientists. I am encouraged that you have included some non-US scientists. I trust that in the future you will look to Canada to assist you in the production of other assessments. It will be important that all data sets and analyses are available to the scientific community who wish to review the conclusions of this assessment - as is the practice with the IPCC. I look forward to seeing the draft in December. Specific CommentsMichael MacCrackenPage 1, Line s 12-13: It should not be implied that different techniques giving different results is necessarily incorrect or wrong. Often the techniques for making measurements are measuring different quantities (directly or indirectly) intended to be representative of different volumes of the atmosphere and for different time samplings. The problem is not so much that there are differences, but that all of the differences have yet to be fully resolved, confirmed, and/or reconciled. William F. O’KeefePage 3, Line 46: Insert the word “potential” in front of the phase “human impact.” Whether human activities have significantly impacted on past climate and the degree to which they might impact on future climate are questions still being actively debated by the scientific community. This debate should be reflected in the phrasing of the summary question. William Fang/Eric HoldsworthPage 4, lines 13-30: Section 6 is titled “Proposed Approach for Evaluation and Communication of Uncertainty and Confidence Levels, Where Applicable.” It states (lines 16-19):
The draft prospectus further indicates that “uncertainties” will be communicated quantatively “in many instances,” but “it is clear that” mathematical estimates “do not reflect the full range of uncertainty.” Thus, the “intent is to follow the protocol developed in the IPCC (2001) assessment and any updates provided by IPCC” (lines 29-30). EEI, in its comments on the general guidelines, raised serious concerns about the use of the term “confidence levels” (see Specific comments, Page 2, Lines 22-25). Since then, it has come to our attention that the Intergovernmental Panel on Climate Change (IPCC), in its cross-cutting themes, indicated that the issue of probabilities needs further examination. Therefore, we call into question the proposal for addressing “confidence levels” in this section 6 by following the “protocol developed” by the IPCC in its third assessment and “any updates provided by IPCC.” Those “updates” could take many months before they are approved by the IPCC. Moreover, the CCSP should not adopt them without an opportunity for further public input. Charles F. KellerPage 4,line 23 It may be important to include developers opinions especially if evaluators come up with much different assessment of reliability of "products". This to avoid, where possible, developers rejecting outright evaluators' assessments as being uninformed. Charles F. KellerPage 5, line 16 this rather tight time constraint assumes that data reliability "evaluators" are already able to make an informed estimate of the uncertaintities since usually there is no such detailed evaluation in the refereed literature excepting that done by the "developers". Is this true? Charles F. KellerPage 6 Line 3-4 ff Since Q. #1 deals with vertical variability of temperature in the troposphere, one might expect to see at least one lead author who is noted for studying this (as evidenced by their cited publications). As excellent as the listed authors are, none seems to have concentrated on this aspect of atmospheric physics. Interestingly one such expert, Steve Sherwood appears below as a lead author for question 2. Might he not be more important as a participant in question 1? Charles F. KellerPage 10, Line 5--Question 4 is a very awkward construction. It is not at all clear to the reader what this question is getting at or what characterization of uncertainties is being questioned. What's going on here? Are you saying that previously published estimates of uncertainties are wrong and therefore are misleading the discussion of whether there are indeed significant vertical differences in temperature trends? How about a different wording such as: "How have estimates of observational and methodological uncertainties limited our understanding of previously reported vertical differences in temperature trends?" William F. O’KeefePage 14, Line 7: Insert the word “potential” in front of the phase “human impact.” Whether human activities have significantly impacted on past climate and the degree to which they might impact on future climate are questions still being actively debated by the scientific community. This debate should be reflected in the phrasing of the summary question. |
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