Sunday, May 6, 2012

3873.txt

cc: Peter Lemke <plemkeatXYZxyz-bremerhaven.de>, Martin Manning <mmanningatXYZxyznoaa.gov>, Susan Solomon <ssolomonatXYZxyznoaa.gov>, ipcc-wg1@al.noaa.gov, k.briffaatXYZxyz.ac.uk
date: Wed, 20 Apr 2005 09:07:27 -0600
from: Kevin Trenberth <trenbertatXYZxyzr.edu>
subject: Re: WG1 LA2 meeting - Overlap cluster A
to: Phil Jones <p.jonesatXYZxyz.ac.uk>

Hi Martin
I agree with what Phil says, but I note that cluster B does not actually have chapter 6 as
part of it. So the question is whether chapter 6 will be involved?. If so then we may
well want to split into 2 parts. Last night I had a quick look at Chap 9 and I am
concerned about redundancy and overlap and conflicts: they are doing some similar things
with observations but maybe different obs, and coming to different conclusions e.g. wrt
things like dimming.
Kevin
Phil Jones wrote:

Dear All,
In addition to Kevin's comments and from a quickish look through parts of Chapters
4, 6 and 9, here are a few suggestions.
First for best use of time, I would suggest that Cluster B gets broken into two
parts.
Basically separating off the overlap with the paleo and instrumental record including
borehole temperatures and glacier length changes from the sea ice/SST,
snow/temperature.
OHC/SST, salinity/precip and SLR etc. The latter can be dealt with by Chs 5, 3 and 4.
The former is really for 6, 3 and 4.
Issues for 3 and 6 are the interface of the instrumental and paleo records,
particularly
how the early 19th century is dealt with. This period of instrumental records is
believed
by many in the paleo community not to exist, but in Europe and a few other regions it
exists back in good order to the late 18th century. The 19th century is, I believe, the
key
to resolving much of the discussion about the millennium. Much more should be made of
this period when comparisons with long forced GCM runs are analyzed. Europe may be a
small continent, but the 200-250 year 'perfect proxy' records (which have all seasons!)
need
to be studied more. As any conclusions relate to Ch 6, the main text should be there,
with
perhaps a box on the early instrumental period in Ch 3.
Somewhat related to the above, Ch 4 has a section on the recent Oerlemans (2005)
work
- attached for reference. Mike Mann sent me a figure (see jpg) comparing this with most
other
reconstructions of parts of the millennium. It seems that this piece of work should be
with
all the others in Ch 6 and not Ch 4. When producing plots like this getting the right
base level
is crucial - not just for Oerlemans' series, but also for the boreholes. Also, the
degree of
smoothing and the y-scale used can easily determine the takeaway message.
Chapter 9 has an interest in both these issues.
Finally, there is one other issue. Do we want to consider having a web site
(distributed?) where
the data for some selected time series can be downloaded from - not just the
smoothed/plotted
series, but on the original timescale as well. This possibly comes back also to a
consistent way
of smoothing time series.
Cheers
Phil
At 08:11 20/04/2005, Peter Lemke wrote:

Dear Martin,
I am also willing to co-chair the cluster B. (As always) Kevin has done a very good job
in listing the most important issues.
Therefore, I have nothing to add at the moment. I will think about this on the weekend.
Best regards,
Peter
Kevin Trenberth schrieb:

Hi Martin
Yes I will do this.
Firstly on cluster A:
I/we have an issue which is: what about changes in radiative forcing from water vapor
(or feedback if you prefer), it is of order 1 W m-2.
So this relates to water vapor changes in chapter 3.
Cluster B: Consistency in observed climate change: atmosphere, ocean, cryosphere. This
may also extend to paleo, chapter 6.
Issues:
*Consistency of:*
* sea ice with SST
* snow cover with snowfall and temperature
* glacier melting and permafrost changes vs temperatures
* borehole temperatures, glacier changes and paleo record
* overlap between paleo record and instrumental record
* salinity vs precipitation
* ocean heat content with SST and surface fluxes
* sea level rise as an integrator: ocean expansion, melting of
land ice, increased water storage on land, and changes in TOA
radiation (presumably led by Chapter 5.)
Issues consist of use of consistent temperature and precipitation records (don't use
NCEP surface temperatures as in Ch 4 CQ).
Points of contention:
1) consistency
2) overlap and redundancy
3) where to place integrated assessment?
* sea level: Chapter 5
* snow, ice, temperature chapter 3 section 3.9
* paleo record vs instrumental chapter 6
* overall view including sea level chapter 3, in 3.9
* T increase (land, SST, subsurface ocean), snow retreat, sea ice
retreat, thinning, freezing season shorter, glacier melt, sea
level rise.
* Precip changes, drought, salinity, ocean currents, P-E, snowfall.
Please see the draft of 3.9.
So in terms of the agenda, the main points are:
1) Ensuring consistency among variables across chapters
2) Agreement on which chapter and what person will handle what, and in particular, that
3.9 will have a look ahead aspect to the chapters that follow.
The above points could all be briefly on the table with the focus on cross-chapter
issues.
Desirable to circulate draft section 3.9 (1 page).
Peter may wish to add or change this?
Regards
Kevin
Martin Manning wrote:

Dear Kevin and Peter
Please find attached our current program for the second Lead Author meeting on May 10 -
12. We will shortly be sending out some more details on the plans for the meeting and
in particular would like to clarify what needs to be done in the Overlap Cluster
meetings shown in the program on Wednesday 11th.
This is to ask if you would be prepared to jointly co-chair the session on Overlap
Cluster B dealing with "Consistency in covering observed climate change" and which will
involve discussion among chapters 3, 4, 5, 9 and 11. The attached program lists, on the
last page, overlap / consistency areas that have been mentioned in the ZOD.
We would really be most grateful for your assistance in this, and if you agree, we would
like to ask that you each to specify what in your view would be the 2 or 3 most
important issues to resolve during the overlap cluster session. We will then use your
input to draw up a specific agenda and circulate agendas for all overlap clusters to all
CLAs prior to the meeting. We hope in this way that we can reach a shared understanding
of the most important overlap and consistency issues and the corresponding key decisions
that will have to be made in Beijing.
I would be grateful if you could let me know whether you are able to help us with this
by Wednesday 20th.
Regards
Martin
--
*Recommended Email address: [1]mmanning@al.noaa.gov
*** Please note that problems may occur with my @noaa.gov address
Dr Martin R Manning, Director, IPCC WG I Support Unit
NOAA Aeronomy Laboratory Phone: +1 303 497 4479
325 Broadway, DSRC R/AL8 Fax: +1 303 497 5628
Boulder, CO 80305, USA

-- ****************
Kevin E. Trenberth e-mail: [2]trenbert@ucar.edu
Climate Analysis Section, NCAR [3]www.cgd.ucar.edu/cas/
P. O. Box 3000, (303) 497 1318
Boulder, CO 80307 (303) 497 1333 (fax)
Street address: 1850 Table Mesa Drive, Boulder, CO 80303

--
****************************************************
Prof. Dr. Peter Lemke
Alfred-Wegener-Institute
for Polar and Marine Research
Postfach 120161
27515 Bremerhaven
GERMANY
e-mail: [4]plemke@awi-bremerhaven.de
Phone: ++49 (0)471 - 4831 - 1751/1750
FAX: ++49 (0)471 - 4831 - 1797
[5]http://www.awi-bremerhaven.de
****************************************************

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 [6]p.jones@uea.ac.uk
NR4 7TJ
UK
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[cid:part1.06010200.08000003@ucar.edu]

--
****************
Kevin E. Trenberth e-mail: [7]trenbert@ucar.edu
Climate Analysis Section, NCAR [8]www.cgd.ucar.edu/cas/
P. O. Box 3000, (303) 497 1318
Boulder, CO 80307 (303) 497 1333 (fax)

Street address: 1850 Table Mesa Drive, Boulder, CO 80303

Embedded Content: Re WG1 LA2 meeting - Overlap c.jpg: 00000001,429c633d,00000000,00000000

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