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Original Articles

Limnological research in the deep southern subalpine lakes: synthesis, directions and perspectives

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Pages 29-66 | Received 24 Nov 2009, Accepted 24 Feb 2010, Published online: 05 Jul 2010

Figures & data

Figure 1. Geographical location of the deep southern subalpine lakes (DSL) in northern Italy.

Figure 1. Geographical location of the deep southern subalpine lakes (DSL) in northern Italy.

Table 1. Morphometric and hydrological characteristics of the deep southern subalpine lakes (DSL) in Northern Italy.

Table 2. Principal limnological studies carried out since 1995 in the deep southern subalpine lakes (DSL). Studies carried out on two or more lakes are reported under ‘DSL’.

Figure 2. Ordination of the DSL and research topics in the correspondence analysis plane defined by the first two axes. Research topics have been coded as in . Gar, Garda; Ise, Iseo; Com, Como; Lug, Lugano, Mag, Maggiore; DSL, deep southern subalpine lakes.

Figure 2. Ordination of the DSL and research topics in the correspondence analysis plane defined by the first two axes. Research topics have been coded as in Table 2. Gar, Garda; Ise, Iseo; Com, Como; Lug, Lugano, Mag, Maggiore; DSL, deep southern subalpine lakes.

Figure 3. Volume-weighted mean lake temperature from the beginning of the 1970s to 2009 (updated from Citation79). (a) Garda; (b) Iseo; (c) Como; (d) Maggiore. Measurements were made during spring, at the time of maximum overturn. Data are smoothed using the LOWESS procedure. Dashed lines show the Theil-Sen slopes of the linear trends. For every temperature series, various statistics have been computed: MK, Mann–Kendall test Citation245; BS-MK, Bootstrap-based MK test with 10000 replications Citation245; TFPW-MK, trend-free pre-whitening procedure (TFPW) and MK test Citation246; TS-slope, Theil-Sen's slope estimates (°C year−1) Citation245.

Figure 3. Volume-weighted mean lake temperature from the beginning of the 1970s to 2009 (updated from Citation79). (a) Garda; (b) Iseo; (c) Como; (d) Maggiore. Measurements were made during spring, at the time of maximum overturn. Data are smoothed using the LOWESS procedure. Dashed lines show the Theil-Sen slopes of the linear trends. For every temperature series, various statistics have been computed: MK, Mann–Kendall test Citation245; BS-MK, Bootstrap-based MK test with 10000 replications Citation245; TFPW-MK, trend-free pre-whitening procedure (TFPW) and MK test Citation246; TS-slope, Theil-Sen's slope estimates (°C year−1) Citation245.

Figure 4. Volume-weighted average concentrations of (a) total phosphorus in the whole lake and (b) dissolved oxygen in the layer below 200 m from the beginning of the 1970s to 2008. The series are based on measurements carried out at the time of maximum overturn during spring (updated from Refs Citation75,Citation76,Citation79).

Figure 4. Volume-weighted average concentrations of (a) total phosphorus in the whole lake and (b) dissolved oxygen in the layer below 200 m from the beginning of the 1970s to 2008. The series are based on measurements carried out at the time of maximum overturn during spring (updated from Refs Citation75,Citation76,Citation79).

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