The Impact of NRC Recommendations on Climate Reconstructions U11B05 - PowerPoint PPT Presentation

1 / 17
About This Presentation
Title:

The Impact of NRC Recommendations on Climate Reconstructions U11B05

Description:

Spaghetti in the Urals. Briffa's Yamal chronology inconsistent with other chronologies; ... Bottom- Treeline at Polar Urals (Shiyatov 1995) One site can affect ... – PowerPoint PPT presentation

Number of Views:78
Avg rating:3.0/5.0
Slides: 18
Provided by: climat6
Category:

less

Transcript and Presenter's Notes

Title: The Impact of NRC Recommendations on Climate Reconstructions U11B05


1
The Impact of NRC Recommendations on Climate
ReconstructionsU11B-05
  • AGU December 2006 Meeting
  • Stephen McIntyre
  • Toronto, Canada
  • www.climateaudit.org/pdf/agu06.ppt

2
NRC Panel and MM
3
Key Recommendations and Findings
  • Precipitation-sensitive proxies e.g.
    moisture-sensitive trees and isotopes in
    tropical ice cores should not be used without
    climatologic justification of any apparent
    proxy-temperature correlation
  • Strip-bark bristlecone and foxtails should be
    avoided.
  • Many reconstructions are based on the same
    datasets and are not independent. Some are not
    robust with respect to removal of individual
    proxies.

4
Plausible...
  • NRC panel used 4 reconstructions as comfort for
    comparing modern-medieval levels, but did verify
    that cited reconstructions met proxy quality
    standards. Medieval-modern relationship reverses
    with trivial and justifiable variations in proxy
    selection.

5
Most MBH proxies are indistinguishable from
high-frequency noise. The pattern comes from
bristlecones.
Left 6 MBH99 proxies. Right top contribution
of proxy classes (proxy type continent) to
MBH reconstruction, bristlecones in red. Bottom
same with each proxy class scaled.
6
Bristlecones and foxtails occupy cold arid niche
Mooney bristlecone pine is responding in gross
terms primarily to a moisture gradient in the
White Mts. Its main competitor is sagebrush.
Lloyd and Graumlich previous winter
precipitation is the most important factor
governing growth variation
7
Underwater medieval trees in the Sierra Nevadas
...
  • Major long-term changes in local hydrology
  • Lakes re-formed only in the Little Ice Age
  • Graumlich late 20th century less remarkable
    for warmth than for high winter precipitation
    totals

8
Bristlecone/foxtail chronologies are
inconsistent with ecological temperature
estimates...
Miller et al 2006 Medieval forests on summits
were typical of forests currently 300-500m
lower medieval annual temperatures were 3.2
deg C warmer than at present. Left Medieval
tree above treeline right- bristlecone and
foxtail ring width chronologies
9
Spaghetti in the Urals
  • Briffas Yamal chronology inconsistent with other
    chronologies
  • Inconsistent with ecological estimates that
    medieval temperatures were 2.5-3.5 deg warmer
  • Top Spaghetti graph showing Briffa 1995
    (black), Briffa 2000 (Yamal red) Polar Urals
    update (Esper 2002 blue)
  • Bottom- Treeline at Polar Urals (Shiyatov 1995)

10
One site can affect a reconstruction
  • Blue Briffa 2000 reconstruction using Yamal
    chronology yellow impact using Polar Urals
    update. Impact on D'Arrigo et al 2006 will be
    similar since 5 of 6 series overlap.

11
dO18 Decreases at Mount Logan and Law Dome
  • No rational basis for attributing Mt Logan and
    Law Dome to circulation changes, while citing
    Guliya and tropical cores as evidence of
    unusual temperature increases
  • Panel did not discuss Law Dome when stating that
    no Antarctic sites show medieval warming

12
Spaghetti Guliya
  • Three different versions of Thompsons 1992
    Guliya dO18 series used in 2006 studies.
    Reconciliation and quality control is a
    prerequisite for statistical analysis. Results
    from all samples need to be archived.

13
Monsoon Proxies used in Temperature Composites
Top Three monsoon proxies used in temperature
composites right journal titles and picture of
Dulan juniper
14
Arbitrary selection of ocean sediment proxies
  • G. Bulloides pattern is not characteristic of
    other high-resolution sediment proxies
  • Many high-resolution ocean proxies show distinct
    MWP, even in Antarctica
  • Dating precision is insufficient to prove or
    disprove synchronization

15
Seeming modern-medieval differential depends on a
very few problematic proxies
  • Bristlecone/foxtail ring width chronologies
  • Selection of Yamal, Siberia ring width chronology
    in preference to updated Polar Urals
  • Use of precipitation or even monsoon wind speed
    proxies in temperature reconstructions
    Thompsons Himalaya ice core isotopes Arabian
    Sea cold water G Bulloides Dulan junipers

16
A Different Spaghetti Recipe
Variations of standard reconstructions using
Polar Urals update instead of Yamal and Sargasso
Sea SST instead of G Bulloides wind speed proxy
and Yakutia instead of problematic
bristlecones/foxtails.
17
Conclusions
  • There are very few proxies that actually
    contribute to seeming modern-medieval
    differential
  • These proxies are used over and over
  • These proxies, especially bristlecones, do not
    meet NRC panel recommendations or reconcile with
    ecological information
  • None of the comfort studies meets NRC panel
    recommendations for proxy quality
Write a Comment
User Comments (0)
About PowerShow.com