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Record #93911:
- #93911
Main publication details
MARC recordHigh frequency ambient sound in the Arctic / David M. Farmer, Sherman R. Waddell.
| Title: | High frequency ambient sound in the Arctic / David M. Farmer, Sherman R. Waddell. |
| Author(s): | Farmer, David M. Waddell, Sherman R. |
| Date: | 1988. |
| Publisher: | Dordrecht: Kluwer Academic Publishers |
| In: | Sea surface sound; natural mechanisms of surface generated noise in the ocean. (1988.), |
| Abstract: | Sound pressure levels recorded in six frequency bands from 50 to 14,500 Hz provide acoustic description of evolving processes of ice cracking and disintegration from 2 April to 7 August 1986 in Dolphin and Union Strait, Canadian Arctic archipelago. In early spring, dominant sources of sound are thermal stress cracking and wind effects. In early June, sound level drops to very low values. Thereafter, progressive deterioration of ice leads to increase in sound levels and short-term variability. These acoustic signatures can be related to satellite and meteorological observations. |
| Notes: | In: Sea surface sound; natural mechanisms of surface generated noise in the ocean / Bryan R. Kerman, ed. Proceedings of the NATO Advanced Research Workshop on Sea Surface Sound: Natural Mechanisms of Surface Generated Noise in the Ocean, held in Lerici, Italy, 15-19 June 1987. |
| Keywords: | 551.32 -- Glaciology. 551.326 -- Floating ice. 534.2 -- Acoustics in ice. E6 -- Glaciology: floating ice. (*60) -- Arctic Ocean and adjacent waters. |
| SPRI record no.: | 93911 |
LDR 01847naa#a2200000#a#4500 001 SPRI-93911 005 20231204161311.0 007 ta 008 231204s1988####ne#ab##|#####|0||#0#eng#d 035 ## ‡aSPRI-93911 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aFarmer, David M. 245 10 ‡aHigh frequency ambient sound in the Arctic /‡cDavid M. Farmer, Sherman R. Waddell. 260 ## ‡aDordrecht :‡bKluwer Academic Publishers,‡c1988. 300 ## ‡ap. 555-563 :‡bill., diags., maps. 490 0# ‡aNATO ASI Series C: Mathematical and Physical Sciences ;‡vVol. 238 500 ## ‡aIn: Sea surface sound; natural mechanisms of surface generated noise in the ocean / Bryan R. Kerman, ed. 500 ## ‡aProceedings of the NATO Advanced Research Workshop on Sea Surface Sound: Natural Mechanisms of Surface Generated Noise in the Ocean, held in Lerici, Italy, 15-19 June 1987. 520 3# ‡aSound pressure levels recorded in six frequency bands from 50 to 14,500 Hz provide acoustic description of evolving processes of ice cracking and disintegration from 2 April to 7 August 1986 in Dolphin and Union Strait, Canadian Arctic archipelago. In early spring, dominant sources of sound are thermal stress cracking and wind effects. In early June, sound level drops to very low values. Thereafter, progressive deterioration of ice leads to increase in sound levels and short-term variability. These acoustic signatures can be related to satellite and meteorological observations. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a534.2 -- Acoustics in ice.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 700 1# ‡aWaddell, Sherman R. 773 0# ‡7nnam ‡aBryan R. Kerman, ed. ‡tSea surface sound; natural mechanisms of surface generated noise in the ocean. ‡dDordrecht : Kluwer Academic Publishers, 1988. ‡wSPRI-93907 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231204