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. 2009 Nov;54(6):2283-2297.
doi: 10.4319/lo.2009.54.6_part_2.2283.

Lakes as sentinels of climate change

Affiliations

Lakes as sentinels of climate change

Rita Adrian et al. Limnol Oceanogr. 2009 Nov.

Abstract

While there is a general sense that lakes can act as sentinels of climate change, their efficacy has not been thoroughly analyzed. We identified the key response variables within a lake that act as indicators of the effects of climate change on both the lake and the catchment. These variables reflect a wide range of physical, chemical, and biological responses to climate. However, the efficacy of the different indicators is affected by regional response to climate change, characteristics of the catchment, and lake mixing regimes. Thus, particular indicators or combinations of indicators are more effective for different lake types and geographic regions. The extraction of climate signals can be further complicated by the influence of other environmental changes, such as eutrophication or acidification, and the equivalent reverse phenomena, in addition to other land-use influences. In many cases, however, confounding factors can be addressed through analytical tools such as detrending or filtering. Lakes are effective sentinels for climate change because they are sensitive to climate, respond rapidly to change, and integrate information about changes in the catchment.

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Figures

Fig. 1
Fig. 1
Long-term behavior of monthly mean near-surface temperatures since 1970 in January (TJan, A–D) and July (TJuly, E–P) in various Northern Hemisphere lakes. (A) and (E) Lake Zürich (Switzerland); (B) and (F) Lake Constance (Germany, Switzerland, Austria); (C) and (G) Lake Washington (Washington); (D) and (H) Lake Tahoe (California, Nevada); (I) Greifensee (Switzerland); (J) Lake Vättern, Edeskvarva basin (Sweden); (K) Lake Mäleren, Görvaln basin (Sweden); (L) Stensjön (Sweden); (M) Müggelsee (Germany); (N) Lake Baikal (Russia); (O) Lake Champlain (Vermont); (P) Blue Chalk Lake (Canada). Monthly means were obtained by spline-interpolating measured temperatures at daily intervals and averaging the results. For each lake, the significance level of the Mann–Kendall test for the existence of a monotonic trend is indicated by one, two, or three asterisks (p < 0.1, p < 0.05, and p < 0.01, respectively) or a dash (no monotonic trend at the p < 0.1 level). The mean rate of change of TJan or TJuly is also given, and the long-term linear trend is illustrated.

References

    1. ACIA . Impacts of a warming Arctic: Arctic climate impact assessment. Cambridge Univ. Press; 2004.
    1. Adrian R, Walz N, Hintze T, Hoeg S, Rusche R. Effects of ice duration on the plankton succession during spring in a shallow polymictic lake. Freshwater Biol. 1999;41:621–623.
    1. Adrian R, Wilhelm S, Gerten D. Life history traits of lake plankton species may govern their phenological response to climate warming. Glob. Change Biol. 2006;12:652–661.
    1. Argyilan EP, Forman SL. Lake level response to seasonal climatic variability in the Lake Michigan–Huron system from 1920 to 1995. J. Great Lakes Res. 2003;29:488–500.
    1. Arhonditsis GB, Brett MT, DeGasperi CL, Schindler DE. Effects of climatic variability on the thermal properties of Lake Washington. Limnol. Oceanogr. 2004;49:256–270.

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