Details

Autor(en) / Beteiligte

• Hakim, Gregory J.
• Emile‐Geay, Julien
• Steig, Eric J.
• Noone, David
• Anderson, David M.
• Tardif, Robert
• Steiger, Nathan
• Perkins, Walter A.

Titel

The last millennium climate reanalysis project: Framework and first results

Ist Teil von

• Journal of geophysical research. Atmospheres, 2016-06, Vol.121 (12), p.6745-6764

Ort / Verlag

Washington: Blackwell Publishing Ltd

Erscheinungsjahr

2016

Link zum Volltext

Quelle

Wiley Online Library

Beschreibungen/Notizen

• An “offline” approach to DA is used, where static ensemble samples are drawn from existing CMIP climate‐model simulations to serve as the prior estimate of climate variables. We use linear, univariate forward models (“proxy system models (PSMs)”) that map climate variables to proxy measurements by fitting proxy data to 2 m air temperature from gridded instrumental temperature data; the linear PSMs are then used to predict proxy values from the prior estimate. Results for the LMR are compared against six gridded instrumental temperature data sets and 25% of the proxy records are withheld from assimilation for independent verification. Results show broad agreement with previous reconstructions of Northern Hemisphere mean 2 m air temperature, with millennial‐scale cooling, a multicentennial warm period around 1000 C.E., and a cold period coincident with the Little Ice Age (circa 1450–1800 C.E.). Verification against gridded instrumental data sets during 1880–2000 C.E. reveals greatest skill in the tropics and lowest skill over Northern Hemisphere land areas. Verification against independent proxy records indicates substantial improvement relative to the model (prior) data without proxy assimilation. As an illustrative example, we present multivariate reconstructed fields for a singular event, the 1808/1809 “mystery” volcanic eruption, which reveal global cooling that is strongly enhanced locally due to the presence of the Pacific‐North America wave pattern in the 500 hPa geopotential height field. Key Points Data assimilation climate field reconstruction skillful against out‐of‐sample instrumental data and proxies Reconstruction skill is highest in the tropics and lowest over Northern Hemisphere land areas Multivariate reconstruction of 1808/1809 volcanic cooling associated with PNA pattern in 500 hPa geopotential height