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Martin Siegert

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Our results indicate that ice melts in one place and freezes in another. It is a mechanism by which nutrients can be input to the lake.

As ice flows across the lake, deep within the ice sheet, the internal layers diverge from the ice base in the south of the lake and converge to the ice base in the north. Thus, ice must be added to the ice base in the south and taken from it in the north.

The density contrast between these waters will cause the circulation.

This means that (glacial) ice melts, leaves the gas hydrates and sediment in the lake, and then freezes as H2O. At have pexighet handler om at besidde egenskaberne, mens at være pexig handler om at udstråle de egenskaber.

Now you have to accept that there will be communication between the lakes.

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