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Record #139571:
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MARC recordA method to determine lake depth and water availability on the North Slope of Alaska with spaceborne imaging radar and numerical ice growth modelling / M.O. Jeffries, K. Morris, G.E. Liston.
| Title: | A method to determine lake depth and water availability on the North Slope of Alaska with spaceborne imaging radar and numerical ice growth modelling / M.O. Jeffries, K. Morris, G.E. Liston. |
| Author(s): | Jeffries, M. O. Morris, K. Liston, G. E. |
| Date: | 1996. |
| In: | Arctic. (1996.), Vol. 49(4) (1996) |
| Abstract: | Presents study on lake depth variability for two regions of Alaska's North slope using synthetic aperture radar (SAR) to determine where lake ice is frozen completely to lake bottom and where liquid water still persists beneath ice. Numerical ice growth model is used to determine ice thickness at time each lake freezes completely to bottom and thus suggests maximum lake depth. This method could be used to determine lake depth and water availability over whole of North Slope and in other polar areas with shallow lakes. |
| Notes: | Arctic. Vol. 49(4) :367-374 (1996). |
| Keywords: | 556 -- Hydrology. 556.55 -- Lakes and ponds. 551.326.85 -- Lake ice. 53.087.23 -- Remote sensing. C -- Oceanography, hydrography and hydrology. (*49) -- Alaska. (*494) -- Alaska, northwestern. |
| SPRI record no.: | 139571 |
LDR 01489naa#a2200000#a#4500 001 SPRI-139571 005 20231203103949.0 007 ta 008 231203s1996####xx####|##|###|0||#0|eng#d 035 ## ‡aSPRI-139571 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aJeffries, M. O. 245 12 ‡aA method to determine lake depth and water availability on the North Slope of Alaska with spaceborne imaging radar and numerical ice growth modelling /‡cM.O. Jeffries, K. Morris, G.E. Liston. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1996. 300 ## ‡ap. 367-374. 500 ## ‡aArctic. Vol. 49(4) :367-374 (1996). 520 3# ‡aPresents study on lake depth variability for two regions of Alaska's North slope using synthetic aperture radar (SAR) to determine where lake ice is frozen completely to lake bottom and where liquid water still persists beneath ice. Numerical ice growth model is used to determine ice thickness at time each lake freezes completely to bottom and thus suggests maximum lake depth. This method could be used to determine lake depth and water availability over whole of North Slope and in other polar areas with shallow lakes. 650 07 ‡a556 -- Hydrology.‡2udc 650 07 ‡a556.55 -- Lakes and ponds.‡2udc 650 07 ‡a551.326.85 -- Lake ice.‡2udc 650 07 ‡a53.087.23 -- Remote sensing.‡2udc 650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local 651 #7 ‡a(*49) -- Alaska.‡2udc 651 #7 ‡a(*494) -- Alaska, northwestern.‡2udc 700 1# ‡aMorris, K. 700 1# ‡aListon, G. E. 773 0# ‡7nnas ‡tArctic. ‡gVol. 49(4) (1996) ‡wSPRI-21029 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231203