In my continuing search for updated dendroclimatological temperature proxies, I started by looking at what had been archived at ITRDB; this has proved to be a very disappointing source of candidates. I’ve re-canvassed some literature for candidate unarchived information. In an email, Connie Woodhouse mentioned that their efforts with upper treeline sites in the U.S. had not yielded any useful results. Our occasional and valued correspondent, Rob Wilson, is very much at the center of upper treeline dendro studies in Canada, making our occasional visits with him all the more valuable. Luckman and Wilson 2003 contains the following useful short synopsis of upper treeline studies:
Dendrochronological studies at upper treeline in the southern Canadian Cordillera have focused on either Vancouver Island (Smith and Laroque, 1998; Laroque and Smith, 1999) or the Canadian Rocky Mountains (Parker and Henoch, 1971; Luckman et al., 1985; 1997; St George and Luckman, 2001). Only two treeline spruce chronologies are available from the large intervening area (Schweingruber, 1988). Recent work in the southern Rockies has established networks of chronology sites using Engelmann spruce (Picea engelmannii Parry), whitebark pine (Pinus albicaulis Engelm) and alpine larch (Larix lyallii Parl) that typically average 300—400 years (Luckman, 1996) but include millennial-length chronologies from each species. Temperature reconstructions have been developed from some of these data using alpine larch (Colenutt, 2000) and Engelmann spruce (Luckman et al., 1985; 1997; St George and Luckman, 2001).
In 1998 a network of 20 new Engelmann spruce chronologies was sampled from sites across southern British Columbia (Figure 1). All sites were at or within 100—200 m of upper treeline, including sites at Kokanee and Kootenay Pass close to the two chronologies sampled in 1983 (Schweingruber, 1988). An additional ring-width chronology was developed for Harts Pass in Washington State from five spruce chronologies sampled in 1992 (Peterson and Peterson, 1994).
Disappointingly, none of the new Canadian measurement data has been archived; only one chronology (the updated Athabaska chronology) has been archived, though oddly enough it does not appear in the ITRDB archive but in the more general WDCP reconstruction archive. As time permits, I plan to post up short excerpts from each of these studies trying to work back as much as possible.
Today I’ll start with Smith and Laroque 1998, the first paper on the list.
I’ve tracked down Laroque and Smith 1998b, Mountain hemlock growth dynamics on Vancouver Island, which is available online, but haven’t tracked down Laroque and Smith 1998a, High-elevation dendroclimatic records from Vancouver Island, which is a workshop presentation. I’ve reported here on Laroque and Smith 1998b, which I presume to be an alternative presentation of the same sites. I’ll try to doublecheck this at some point and, if this assumption is misplaced, I’ll note that here. In the meantime, the sites described in Laroque and Smith 1998b are all high-latitude Vancouver Island sites and appear to be pertinent to the brief survey in Wilson and Luckman 2003.
In 1994, Laroque and Smith sampled four Vancouver Island sites: Circle, Canyon, Milla Lake, Delight Lake. (See map in link). Three of the sites were above 1500 m; the latter two sites were within a km of Aureole ice field. None of the measurement data has been archived, but it is only 9 years since the study.
The authors report that ring widths are sensitive to changing climate, but describe a complicated response surface in which growth is maximized in cool summers with a small snowpack, but with a secondary and much lesser maximum in warm summers with a large snowpack. Laroque and Smith:
the radial growth of mountain hemlock trees growing at high elevation on Vancouver Island are sensitive to changing climate … the greatest increments of radial growth occurred during cool summers that began with a shallow snowpack, while the least amount of radial growth occurred during seasons that began with below normal snowpacks and ended with very warm summer air temperatures (Figure 3). Significantly, our analyses demonstrated that when the seasonal snowpacks exceeded 4 m in depth, radial growth was significantly reduced, regardless of the growing season temperature (Figure 3).
Here is the diagram of their response surface and you can see how complex the relationship between ring width and temperature-snowpack is:
They provided the following graphic for their ring width chronology (it’s smoothed and is the higher; the authors show an El Nino chronology for comparison). It is obviously impossible to inverting the ring width chronology to obtain a temperature estimate using linear methods (such as principal components, rotated principal components or regression) and the authors did not do so in this particular article. All we can say at this point is that Laroque and Smith 1998b do not show a HS-shape signal and, to that extent, do not serve as evidence for the IPCC SPM claim that updated studies provide “additional data showing coherent behaviour across multiple indicators in different parts of the world.” I’m not saying that this data is relevant to vexed issues such as the MWP; I’m merely canvassing dendroclimatological literature (other than that from the main players on the Hockey Team) to see if it supports the SPM claim.
I’ll post up some notes on the other upper treeline articles over the next few days.
Smith, D.J. and Laroque, C.P. 1998a: High-elevation dendroclimatic records from Vancouver Island. In MacIver, D.C. and Meyer, R.E., editors, Proceedings of the Workshop on Decoding Canada’s Environmental Past: Climate Variations and Biodiversity Change during the Last Millennium, Downsview: Atmospheric Environment Service, 33—44
Smith, D.J.; and Laroque, C.P. 1998b. Mountain hemlock growth dynamics on Vancouver Island. Northwest Science 72 (Special Issue 2): 67-70. 