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Record #204767:

Surface reflectance characteristics of Langjökull, Iceland / Ed Pope.

Title: Surface reflectance characteristics of Langjökull, Iceland / Ed Pope.
Author(s): Pope, Ed.
Date: 2013.
Abstract: Uses various retrieval methods to derive broadband surface albedo from ATM, ETM+ and MODIS radiance data collected during August 2007. Dataset and transect analyses show that most precise methods are FLAASH (ATM), and dark pixel or 6S atmospheric correction (ETM+). MODIS data was in broad agreement, but with significant differences depending on spatial resolution and extent, and reduced correlation for larger sample size. At smallest scale, bias towards representing certain areas in individual pixels prevented ETM+ and MODIS imagery from averaging highly variable surfaces. Low resolution instruments overestimated albedo in accumulation area, greatly underestimated it in firn zone, and struggled to capture variability in ablation zone. Favours ETM+ imagery for surface albedo monitoring as most correlated with ATM data.
Notes:

Unpublished thesis submitted in partial fulfilment of M.Phil. in Polar Studies, University of Cambridge.

Keywords: 551.32 -- Glaciology.
551.324.24 -- Ice sheets and caps: Langjökull.
551.321 -- Glaciological methods and instruments.
53.087.23 -- Remote sensing.
551.324.414 -- Land ice, radiation to and from.
E5 -- Glaciology: land ice.
(*35) -- Iceland.
Location(s): SCO: SPRI-THE: 2013[Pop]
SPRI record no.: 204767

MARCXML

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007 ta
008 240419s2013####xx#ab##|#m###|0||#0#eng#d
035 ## ‡aSPRI-204767
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100 1# ‡aPope, Ed.
245 10 ‡aSurface reflectance characteristics of Langjökull, Iceland /‡cEd Pope.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2013.
300 ## ‡a116 p. :‡bill., diags., tables, maps ;‡c30 cm.
500 ## ‡aUnpublished thesis submitted in partial fulfilment of M.Phil. in Polar Studies, University of Cambridge.
520 3# ‡aUses various retrieval methods to derive broadband surface albedo from ATM, ETM+ and MODIS radiance data collected during August 2007. Dataset and transect analyses show that most precise methods are FLAASH (ATM), and dark pixel or 6S atmospheric correction (ETM+). MODIS data was in broad agreement, but with significant differences depending on spatial resolution and extent, and reduced correlation for larger sample size. At smallest scale, bias towards representing certain areas in individual pixels prevented ETM+ and MODIS imagery from averaging highly variable surfaces. Low resolution instruments overestimated albedo in accumulation area, greatly underestimated it in firn zone, and struggled to capture variability in ablation zone. Favours ETM+ imagery for surface albedo monitoring as most correlated with ATM data.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324.24 -- Ice sheets and caps: Langjökull.‡2udc
650 07 ‡a551.321 -- Glaciological methods and instruments.‡2udc
650 07 ‡a53.087.23 -- Remote sensing.‡2udc
650 07 ‡a551.324.414 -- Land ice, radiation to and from.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*35) -- Iceland.‡2udc
852 7# ‡2camdept‡bSCO‡cSPRI-THE‡h2013[Pop]‡9Create 1 item record‡0Migrate
916 ## ‡a148466 -- 2013/09/24 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240419 ‡bJW