@ARTICLE{Angiel_Marek_Heat_1994,
 author={Angiel, Marek},
 volume={vol. 15},
 number={No 1-2},
 journal={Polish Polar Research},
 pages={51-70},
 howpublished={online},
 year={1994},
 publisher={Polish Academy of Sciences},
 publisher={Committee on Polar Research},
 abstract={Research in Hornsund (SW Spitsbergen) aimed to determine time distribution of heat flux in various soils of Arctic periglacial zone in spring and summer. Typical soils were analysed: tundra gleyey cryogenic soil (Pergelic Cryaquent), tundra peaty soil (Pergelic Histosot) and arctic desert soil (Pergelic Cryorthent). Research sites were located in low plains not covered with ice, near a sea, at 7—13 m a.s.l. Heat flux in soils was measured and recorded automatically every 60 s throughout a whole observation period and concurrently at three sites. In spring and summer intensive heat accumulation was observed in all examined soils. Independently on the weather, a cryogenic gleyey soil received greatest heat throughout a day. Environmental conditions have distinct influence on heat resources in soils.},
 type={Article},
 title={Heat flux in selected polar soils in spring and summer (Hornsund, Spitsbergen)},
 URL={http://ochroma.man.poznan.pl/Content/111015/PDF-MASTER/1994-1-2_051-070.pdf},
 keywords={Arctic, Spitsbergen, heat flux in soil, periglacial soils},
}