j.pociask/d4.pdf · 76 Water from snow cover and permafrost thawing predominates in the water...

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Transcript of j.pociask/d4.pdf · 76 Water from snow cover and permafrost thawing predominates in the water...

Page 1: j.pociask/d4.pdf · 76 Water from snow cover and permafrost thawing predominates in the water circulation and in the balance of the non-glaciated areas of Spitsbergen.
Page 2: j.pociask/d4.pdf · 76 Water from snow cover and permafrost thawing predominates in the water circulation and in the balance of the non-glaciated areas of Spitsbergen.
Page 3: j.pociask/d4.pdf · 76 Water from snow cover and permafrost thawing predominates in the water circulation and in the balance of the non-glaciated areas of Spitsbergen.
Page 4: j.pociask/d4.pdf · 76 Water from snow cover and permafrost thawing predominates in the water circulation and in the balance of the non-glaciated areas of Spitsbergen.
Page 5: j.pociask/d4.pdf · 76 Water from snow cover and permafrost thawing predominates in the water circulation and in the balance of the non-glaciated areas of Spitsbergen.
Page 6: j.pociask/d4.pdf · 76 Water from snow cover and permafrost thawing predominates in the water circulation and in the balance of the non-glaciated areas of Spitsbergen.
Page 7: j.pociask/d4.pdf · 76 Water from snow cover and permafrost thawing predominates in the water circulation and in the balance of the non-glaciated areas of Spitsbergen.
Page 8: j.pociask/d4.pdf · 76 Water from snow cover and permafrost thawing predominates in the water circulation and in the balance of the non-glaciated areas of Spitsbergen.
Page 9: j.pociask/d4.pdf · 76 Water from snow cover and permafrost thawing predominates in the water circulation and in the balance of the non-glaciated areas of Spitsbergen.
Page 10: j.pociask/d4.pdf · 76 Water from snow cover and permafrost thawing predominates in the water circulation and in the balance of the non-glaciated areas of Spitsbergen.
Page 11: j.pociask/d4.pdf · 76 Water from snow cover and permafrost thawing predominates in the water circulation and in the balance of the non-glaciated areas of Spitsbergen.

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