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Record #197903:
- #197903
Main publication details
MARC recordOccurrence of synoptic flaw leads of sea ice in the Gulf of Finland / Ove Pärn, Jari Haapala.
| Title: | Occurrence of synoptic flaw leads of sea ice in the Gulf of Finland / Ove Pärn, Jari Haapala. |
| Author(s): | Pärn, Ove. Haapala, Jari. |
| Date: | 2011. |
| In: | Boreal Environment Research. (2011.), Vol. 16(1) (2011) |
| Abstract: | Analyzes flaw lead occurrence in Gulf of Finland using ice charts of Estonian Meteorological and Hydrological Institute covering years 1971-2007 and Helsinki multi-category sea-ice model. Reports flaw leads formed almost everywhere along fast-ice edge when moderate or strong winds act, with winds from W, NW, N and S sectors generating rather uniform lead pattern, thus facilitating navigation in ice. On average, flaw leads are most common in Estonian coastal region, where occurrence is typically 10%-30%. During severe winters when northerly winds are more frequent flaw leads are also common in Finnish coastal region. |
| Notes: | Boreal Environment Research. Vol. 16(1) :71-78 (2011). |
| Keywords: | 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.33 -- Leads. 551.556 -- Wind, effects of. 519.673 -- Modelling. 551.326.124 -- Floating ice, bulletins and charts. 551.326.03 -- Floating ice, forecasting. 656.61.052 -- Seamanship. E6 -- Glaciology: floating ice. (*3) -- Arctic regions. (*61) -- North Atlantic Ocean. (*611) -- Baltic Sea. |
| SPRI record no.: | 197903 |
LDR 01790naa#a2200000#a#4500 001 SPRI-197903 005 20231129113032.0 007 ta 008 231129s2011####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-197903 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aPärn, Ove. 245 10 ‡aOccurrence of synoptic flaw leads of sea ice in the Gulf of Finland /‡cOve Pärn, Jari Haapala. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2011. 300 ## ‡ap. 71-78 :‡bill., diags., table, maps. 500 ## ‡aBoreal Environment Research. Vol. 16(1) :71-78 (2011). 520 3# ‡aAnalyzes flaw lead occurrence in Gulf of Finland using ice charts of Estonian Meteorological and Hydrological Institute covering years 1971-2007 and Helsinki multi-category sea-ice model. Reports flaw leads formed almost everywhere along fast-ice edge when moderate or strong winds act, with winds from W, NW, N and S sectors generating rather uniform lead pattern, thus facilitating navigation in ice. On average, flaw leads are most common in Estonian coastal region, where occurrence is typically 10%-30%. During severe winters when northerly winds are more frequent flaw leads are also common in Finnish coastal region. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.33 -- Leads.‡2udc 650 07 ‡a551.556 -- Wind, effects of.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡a551.326.124 -- Floating ice, bulletins and charts.‡2udc 650 07 ‡a551.326.03 -- Floating ice, forecasting.‡2udc 650 07 ‡a656.61.052 -- Seamanship.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*61) -- North Atlantic Ocean.‡2udc 651 #7 ‡a(*611) -- Baltic Sea.‡2udc 700 1# ‡aHaapala, Jari. 773 0# ‡7nnas ‡tBoreal Environment Research. ‡gVol. 16(1) (2011) ‡wSPRI-140857 916 ## ‡a2011/10/12 -- RF 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231129 ‡bRF