SPRI library catalogue
View a record
Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.
Please search for material in iDiscover for up-to-date information about the library collection.
Record #104148:
Theoretical estimates of light reflection and transmission by spatially complex and temporally varying sea ice covers / Donald K. Perovich.
Title: | Theoretical estimates of light reflection and transmission by spatially complex and temporally varying sea ice covers / Donald K. Perovich. |
Author(s): | Perovich, Donald K. |
Date: | 1990. |
In: | Journal of Geophysical Research. (1990.), Vol. 95(C6) (1990) |
Abstract: | Uses two-stream, multilayer radiative transfer model in wavelength region from 400 to 1000 nm. Ice cover is characterized as layered medium composed of selections from nine distinct snow and ice types, and three case studies are presented. Results suggest that small-scale horizontal variations in snow depth and ice thickness can cause light transmission to change over 3 orders of magnitude. Dramatic changes in reflection and transmission are predicted during early melt season as ice evolves from opaque, snow-covered medium to translucent bare or ponded ice. Implications for remote sensing. |
Notes: | Journal of Geophysical Research. Vol. 95(C6) :9557-9567 (1990). |
Keywords: | 551.326.7 -- Sea ice. 551.326 -- Floating ice. 535 -- Optics, light. 53.087.23 -- Remote sensing. 551.32 -- Glaciology. E6 -- Glaciology: floating ice. |
SPRI record no.: | 104148 |
LDR 01497naa#a2200000#a#4500 001 SPRI-104148 005 20231207192347.0 007 ta 008 231207s1990####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-104148 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aPerovich, Donald K. 245 10 ‡aTheoretical estimates of light reflection and transmission by spatially complex and temporally varying sea ice covers /‡cDonald K. Perovich. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 9557-9567 :‡bill., diags., tables. 500 ## ‡aJournal of Geophysical Research. Vol. 95(C6) :9557-9567 (1990). 520 3# ‡aUses two-stream, multilayer radiative transfer model in wavelength region from 400 to 1000 nm. Ice cover is characterized as layered medium composed of selections from nine distinct snow and ice types, and three case studies are presented. Results suggest that small-scale horizontal variations in snow depth and ice thickness can cause light transmission to change over 3 orders of magnitude. Dramatic changes in reflection and transmission are predicted during early melt season as ice evolves from opaque, snow-covered medium to translucent bare or ponded ice. Implications for remote sensing. 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a535 -- Optics, light.‡2udc 650 07 ‡a53.087.23 -- Remote sensing.‡2udc 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 95(C6) (1990) ‡wSPRI-35252 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231207