Research Article
Variability of Water Chemistry in Tundra Lakes, Petuniabukta Coast, Central Spitsbergen, Svalbard
Table 1
Lake basins and catchment characteristics of tundra lakes.
| Name | Latitude | Longitude | Altitude | Surface catchment area | Water areaa | Max depth | Distance from sea | Outflow | Percent of vegetation | deg N | deg E | m a.s.l. | m2 | m | — | % |
| Lake I | 78°42.11′ | 16°36.60′ | 4 | 13690 | 1 112 | 0.51 | 80 | Episodic in- and outflow | 90 | Lake II | 78°42.16′ | 16°36.95′ | 5 |
9540b | 596 | 0.22 | 160 | Episodic outflow | 90 | Lake III | 78°42.18′ | 16°36.88′ | 5 | 386 | 0.13 | 160 | Episodic in- and outflow | 90 | Lake IV | 78°42.58′ | 16°37.04′ | 9 | 34126 | 5579 | 0.53 | 800 | Isolated | 60 |
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aStatus as measured on July 9, 2001.
bHigh water level in lakes II and III leads to the connection of lakes forming one lake {II/III}.
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