樹木年輪が90年前からの温暖化の影響を明らかに(Tree rings from Gaspésie mountains reveal effects of global warming dating back almost a century)

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2025-04-01 コンコルディア大学

コンコルディア大学の研究チームは、ガスペジー山脈のサントアンヌ川周辺で採取した樹木の年輪を分析し、過去約200年間の積雪量の変動を明らかにしました。その結果、1937年以降、春の雪解け水の流量が顕著に減少しており、これは地球温暖化による冬季の積雪量減少を示唆しています。この減少は、水資源管理や地域の生態系に重要な影響を及ぼす可能性があります。

<関連情報>

大西洋沿岸の年輪復元ギャップを埋める: カナダ、ケベック州ガスペジ、サントアンヌ川の195年にわたる成長期流量記録 Filling the Atlantic coastal tree-ring reconstruction gap: A 195-year record of growing season discharge of the Sainte-Anne River, Gaspésie, Québec, Canada

A.V. Pace, J.-M. St-Jacques, D.D. Noel, G. Fortin
Journal of Hydrology: Regional Studies  Available online: 11 February 2025
DOI:https://doi.org/10.1016/j.ejrh.2025.102229

Graphical Abstract

樹木年輪が90年前からの温暖化の影響を明らかに(Tree rings from Gaspésie mountains reveal effects of global warming dating back almost a century)

Highlights

  • Fills gap in coastal tree-ring based river reconstructions between 41°N and 53°N.
  • Adds fifth river to the four existing river basin reconstructions of Atlantic coast.
  • Found decline in extreme May-July flows since 1937, hence recent snowpack decline.
  • Decadal periods of below-mean MJJ flows more likely than long above-mean flows.
  • Shows long-term hydrological connections all along eastern continental margin.

Abstract

Study region
We present a coastal river reconstruction between the Hudson River and north-central Québec, filling a substantial hiatus between 41° N and 53° N along the Atlantic North American margin, and adding to the four existing Atlantic coastal river basins with reconstructions.

Study focus
This study produced a 195-year tree-ring based reconstruction of growing season flow of the Sainte-Anne River, Gaspésie, Québec, Canada. Our nested reconstruction (maximum R2 = 0.53, maximum RE = 0.32) was based upon eight site chronologies where snowpack limits the length of the growing season.

New hydrological insights for the region
We found declining extreme May-July flows since 1937, suggesting a reduction of snowpack in this alpine region in the northern Appalachians. Our Gaspésie reconstruction showed droughts and pluvials in common with multi-centennial river/moisture reconstructions along the Atlantic Seaboard from New York, Delaware and Maryland and from north-central Québec. A principal components analysis (PCA) and correlation analysis with GRUN (the 5°x5° gridded multi-model ensemble of runoff of Ghiggi et al. (2019. Earth Syst. Sci. Data. 11, (1655–1674) showed common modes of variability through-out this broader region. While energy-limited tree-ring chronologies are well-known in western North America, they are poorly known in eastern North America. We found energy-limited snow proxy sites in this region noted for its high snowfall. This reconstruction may prove useful for wildlife, fisheries and hydroelectric reservoir management.

1900環境一般
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