cc: Kevin Trenberth date: Fri Feb 4 17:28:06 2005 from: Phil Jones subject: RE: [Ch3-cas] [Fwd: Zero order draft of Chapter 3, AR4, IPCC] to: "Folland, Chris" Chris, Thanks. If you can persuade him to send comments a little more constructively following Kevin's guidelines then please do. I think being on the CCSP has been a little of an eye opener for Peter. Some of the email exchanges have been vitriolic - I had a selection sent to me the other day. I'll also talk to Peter in Chicago in 2 weeks time. Cheers Phil At 17:06 04/02/2005, you wrote: Dear Phil I am sorry that Peter was so aggressive rather than just sharp. Not really like that as you know. I think he got overenthusiastic because of the nature of some of the CCSP exchanges on vertical temperature trends between other scientists which have not helped the cause of gentlemanly conduct or clear thinking for that matter. Not a good example! The job of an IPCC reviewer at the ZOD stage is to make positive suggestions to help the Strawman along and not to be too critical. In the IPCC TAR at the ZOD stage we were fortunate that this was realised, though we did try and create this atmosphere in covering emails. I will have a look at the chapter soon. Cheers Chris Professor Chris Folland Head of Climate Variability Research Global climate data sets are available from [1]http://www.hadobs.org Met Office, Hadley Centre, Fitzroy Rd, Exeter, Devon EX1 3PB United Kingdom Email: chris.folland@metoffice.gov.uk Tel: +44 (0)1392 886646 Fax: (in UK) 0870 900 5050 (International) +44 (0)113 336 1072)Kevin, Phil et al., > >my substantive comments on the upper-air portion only. Before I give >specific comments below I have some over-arching comments: > >This draft and the CCSP report seem at best tangential - is this >desirable or sensible? > >There is little effective communication in the main text of the >uncertainty that is inherent in these measures due to the poor quality >of the underlying data and metadata and to the choices made - >"structural uncertainty". It seems that a decision has been made that >RSS and the Fu et al. method are "right" or at least "most right" and >this is what we will put forward as gospel truth almost. Other datasets >are given a cursory once over almost. This completely ignores >legitimate concerns that "structural uncertainty" is large aloft - >seemingly reasonable choices made as to how you homogenise and then >analyse the data can have very large effects. This is not at all >clearly communicated in the current draft. > >The essential distilled message that I think the analysis of UA >temperatures has left us since the TAR, and what this chapter should >say, is: > >"Independent efforts to create climate records from satellite and >radiosonde records since the TAR have served to illuminate previously >unrecognised uncertainties in temperature evolution aloft (Seidel et >al., 2004, Thorne et al., 2005). Further, choices in post-processing >(e.g. Fu et al., 2004) may help to clarify satellite retrievals, but >legitimate concerns remain (Thorne and Tett, 2004, Spencer et al., >2005) and other equally plausible approaches should be actively >considered. Our increased understanding of trend uncertainty aloft >means that we can no longer dismiss warming aloft of similar or greater >magnitude than at the surface over the satellite record. Nor can we >discount a relative cooling aloft. Uncertainties are largest in the >tropics and Southern Hemisphere high latitudes where radiosonde >coverage is poorest. Obviously, the climate has only evolved along a >single pathway. Therefore a major challenge to the climate community is >to refine our range of estimates." > >This is what CCSP effectively says. > >What, rightly or wrongly, I get out of the current draft on an initial >read is: > >"We don't like UAH. We don't believe radiosondes over the satellite >period, but do over the longer period (paradox). We believe Fu et al. >is correct. There is no longer any problem whatsoever." > >I don't think this simple message is actually remotely supported by the >science. Therefore at the very least efforts are required to balance >the text so that this is not the message communicated. I don't think we >should be scared of admitting that we just don't know, if indeed we >just don't know (which I believe is a fair reflection of the state of >the science). > >Specific comments: > >p.23 lines 13-14 and 53-57 and p.24 lines 1-6. I disagree strongly with >these as written. I do not believe that Fu et al. weightings is some >panacea nor that the "cancellation" works on all space and timescales >(the statement needs to be *proved* it cannot be accepted as an article >of faith - that is not the way science works). I'd be amazed if it did. >The reservations raised in the peer reviewed literature need to be >better articulated here for the document to be fair and balanced. I >guess this whole area will evolve significantly over the next 12 months >or so though. > >General concern: In the TAR we used 20N to 20S to define the tropics - >here (Table 3.4.1.b) you use 30N to 30S. I'd suggest 20-20 is >physically more logical and has backward compatablity and should be >used. This is a recommendation of the Exeter workshop report queued for >review in BAMS. Regardless, you need to alight on a single definition >of these regions here and elsewhere in the report and stick to it. If >you look at zonal mean profiles from any UA dataset then 20-20 shows >marked trend changes N and S of it (greater warming) so using 30-30 >gives a chance of a fools gold scenario arising. > >In Table 3.4.1.b TLT is the acronym used in Christy et al. 2003 for >T2LT >- this may very well cause confusion. Admittedly I was only scanning the >tables but I thought that this claimed there was a RSS 2LT channel >equivalent! > >Page 26 lines 28-37. This is at significant odds with the CCSP report >conclusions as currently written. Much of this relates to the relative >weighting being given to the Fu et al. approach by the different author >teams. It will seem very odd to a policy maker to read two such >disparate threads. I particularly dislike the use on line 30 of "when >the stratospheric influence is properly taken into account (Fu et al., >2004a)". How can we say it is properly taken into account that way? >There are a very large population of plausible approaches that could be >taken and to date we have two - a "physical" 2LT and a statistical >T850-300. That is grossly insufficient to make bold statements >regarding one of them properly taking the effect into account. Again, >this needs balance and caveats on the Fu et al. technique until we >resolve unanswered questions. Likewise, T2LT has not been proven to be >untenable in the peer reviewed press - so you cannot make this >statement. My feeling is that we are missing a significant opportunity >here to outline the considerable uncertainty in evolution aloft in >favour of deciding one subset of approaches is right and presenting >this as gospel truth. I am very uncomfortable with this. As I said it >is at significant odds with CCSP. > >page 26. para starting on line 46. Seems almost an afterthought. For >HadAT (at least, but as they are so highly correlated, also highly >likely LKS) the long-term trend in the tropics is entirely an artifact >of the regime shift - if you split time periods then pre- and post-1979 >have negative trends and the whole period has a strong positive trend. >So to state boldly that trends agree and therefore all is well is again >our living in a fools paradise. It is true, but it just shows that >trend metrics are very dangerous beasties and should be handled with >care. The Seidel and lanzante paper should also be quoted here. > >page 68. Bullets on line 15, line 19, and line 31. Again, my concern >here is that these are far too narrow and you are effectively claiming >that one approach is right. Really refers back to my earlier points. >This is painting a light fuzzy grey as black when I don't believe the >science to date supports such an interpretation. > >Page 110, line 55. Containing 676 stations (not CDRs). > >Page 111, line 31 The Thorne et al. referenced is a paper under review >at BAMS that you don't have in your current reference list. Reference >is: Causes of differences in observed climate trends Peter W. Thorne, >David E. Parker, John R. Christy, Carl A. Mears > >Common question 3.2. You'll be unsurprised to hear that I think this >paints too rosy a picture of our understanding the vertical structure >of temperature changes. Observations do not show rising temperatures >throughout the tropical troposphere unless you accept one single study >and approach and discount a wealth of others. This is just downright >dangerous. We need to communicate the uncertainty and be honest. > >Phil, hopefully we can find time to discuss these further if necessary >either in Chicago or when I visit in March (has a date been decided >yet?). > >I'll be away from three weeks from today and unable to access this >email account. If we need to iterate further I can be reached >(intermittently) on peterwthorne@btinternet.com but will be fairly busy >and then on holiday in the middle week. > >Peter >-- >Peter Thorne Climate Research Scientist >Hadley Centre for climate prediction and research >Met Office, FitzRoy Road, Exeter, EX1 3PB >Tel:+44 1392 886552 Fax:+44 1392 885681 [3]http://www.hadobs.org Prof. Phil Jones Climatic Research Unit Telephone +44 (0) 1603 592090 School of Environmental Sciences Fax +44 (0) 1603 507784 University of East Anglia Norwich Email p.jones@uea.ac.uk NR4 7TJ UK ------------------------------------------------------------------------ ---- Prof. Phil Jones Climatic Research Unit Telephone +44 (0) 1603 592090 School of Environmental Sciences Fax +44 (0) 1603 507784 University of East Anglia Norwich Email p.jones@uea.ac.uk NR4 7TJ UK ----------------------------------------------------------------------------