FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2058197119> ?p ?o ?g. }

• W2058197119 endingPage "91" @default.
• W2058197119 startingPage "77" @default.
• W2058197119 abstract "Spatial and temporal variations of surface albedo on the North Slope of Alaska were investigated using both ground-based tower measurements and satellite remote sensing data. Ground-based measurements of incident and reflected solar radiation at several stations along the Dalton Highway over the period 1985–98 are used to determine in situ surface albedo. Advanced Very High Resolution Radiometer (AVHRR)-derived surface albedo were obtained from AVHRR Polar Pathfinder products, available from the National Snow and Ice Data Center, using a modified cloud mask. AVHRR-derived surface albedo agrees closely with in situ measurements. Results from this study indicate that surface albedo varies from greater than 0.9 for a snow-covered land surface under overcast conditions to less than 0.1 for a wet tundra land surface. Five distinct temporal periods are discerned, based on seasonal variations of surface albedo: winter stationary, spring snowmelt, postsnowmelt, summer stationary, and autumn freeze-up periods. Spatially, the North Slope is divided into three zones based on patterns of seasonal variation in surface albedo. A mountain zone is along the ranges and slopes of the Brooks Range, with elevations above 1000 m. When compared with the other two zones, surface albedo in this zone is the lowest in winter, varying from 0.4 to 0.7, and relatively high in summer, from 0.15 to 0.2. The foothills zone is along the foothills of the Brooks Range, with elevations from 300 to 1000 m. Surface albedo is relatively high in this zone in winter (0.8) and the highest in summer (0.2). Surface albedo in this zone changes very rapidly from 0.8 to 0.2 within a couple of weeks in spring. The coastal zone is along the Arctic coastal plain, with elevations lower than 300 m. Coastal zone surface albedo is the highest in winter (>0.8) and the lowest in summer (<0.15). This study suggests that the heat island effect in the vicinity of Barrow, Alaska, is very minimal. Progressive earlier snow cover disappearance at the Barrow National Weather Service station may be an indication of regional spring warming. This study also suggests that snow surface albedo in land surface models should be treated differently for snow at high latitudes as compared with snow in midlatitudes, especially during winter months." @default.
• W2058197119 created "2016-06-24" @default.
• W2058197119 creator A5021721475 @default.
• W2058197119 creator A5043556097 @default.
• W2058197119 creator A5050673674 @default.
• W2058197119 creator A5073975634 @default.
• W2058197119 creator A5083178383 @default.
• W2058197119 creator A5083965618 @default.
• W2058197119 date "2003-02-01" @default.
• W2058197119 modified "2023-09-28" @default.
• W2058197119 title "Ground-Based and Satellite-Derived Measurements of Surface Albedo on the North Slope of Alaska" @default.
• W2058197119 cites W1614313607 @default.
• W2058197119 cites W1626696792 @default.
• W2058197119 cites W1654408166 @default.
• W2058197119 cites W170345685 @default.
• W2058197119 cites W173621861 @default.
• W2058197119 cites W1966205080 @default.
• W2058197119 cites W1987540621 @default.
• W2058197119 cites W1989241928 @default.
• W2058197119 cites W1991095279 @default.
• W2058197119 cites W1991118457 @default.
• W2058197119 cites W1999691109 @default.
• W2058197119 cites W2004399829 @default.
• W2058197119 cites W2023431650 @default.
• W2058197119 cites W2033061003 @default.
• W2058197119 cites W2044870224 @default.
• W2058197119 cites W2047207020 @default.
• W2058197119 cites W2052559311 @default.
• W2058197119 cites W2052857711 @default.
• W2058197119 cites W2054732143 @default.
• W2058197119 cites W2061048580 @default.
• W2058197119 cites W2068130621 @default.
• W2058197119 cites W2071980890 @default.
• W2058197119 cites W2072896432 @default.
• W2058197119 cites W2077078481 @default.
• W2058197119 cites W2080604996 @default.
• W2058197119 cites W2084503386 @default.
• W2058197119 cites W2085550196 @default.
• W2058197119 cites W2094270001 @default.
• W2058197119 cites W2110558516 @default.
• W2058197119 cites W2159780131 @default.
• W2058197119 cites W2177198044 @default.
• W2058197119 cites W2177249406 @default.
• W2058197119 cites W2469185797 @default.
• W2058197119 cites W2605334580 @default.
• W2058197119 cites W4230924418 @default.
• W2058197119 cites W4235207478 @default.
• W2058197119 cites W4243744771 @default.
• W2058197119 doi "https://doi.org/10.1175/1525-7541(2003)004<0077:gbasdm>2.0.co;2" @default.
• W2058197119 hasPublicationYear "2003" @default.
• W2058197119 type Work @default.
• W2058197119 sameAs 2058197119 @default.
• W2058197119 citedByCount "12" @default.
• W2058197119 countsByYear W20581971192012 @default.
• W2058197119 countsByYear W20581971192013 @default.
• W2058197119 countsByYear W20581971192015 @default.
• W2058197119 countsByYear W20581971192021 @default.
• W2058197119 crossrefType "journal-article" @default.
• W2058197119 hasAuthorship W2058197119A5021721475 @default.
• W2058197119 hasAuthorship W2058197119A5043556097 @default.
• W2058197119 hasAuthorship W2058197119A5050673674 @default.
• W2058197119 hasAuthorship W2058197119A5073975634 @default.
• W2058197119 hasAuthorship W2058197119A5083178383 @default.
• W2058197119 hasAuthorship W2058197119A5083965618 @default.
• W2058197119 hasBestOaLocation W20581971191 @default.
• W2058197119 hasConcept C114793014 @default.
• W2058197119 hasConcept C127313418 @default.
• W2058197119 hasConcept C127413603 @default.
• W2058197119 hasConcept C142362112 @default.
• W2058197119 hasConcept C146978453 @default.
• W2058197119 hasConcept C153294291 @default.
• W2058197119 hasConcept C19269812 @default.
• W2058197119 hasConcept C195452092 @default.
• W2058197119 hasConcept C195886398 @default.
• W2058197119 hasConcept C197046000 @default.
• W2058197119 hasConcept C205649164 @default.
• W2058197119 hasConcept C2777480484 @default.
• W2058197119 hasConcept C39432304 @default.
• W2058197119 hasConcept C49204034 @default.
• W2058197119 hasConcept C52119013 @default.
• W2058197119 hasConcept C554144382 @default.
• W2058197119 hasConcept C62649853 @default.
• W2058197119 hasConcept C64649846 @default.
• W2058197119 hasConcept C73329638 @default.
• W2058197119 hasConcept C91586092 @default.
• W2058197119 hasConceptScore W2058197119C114793014 @default.
• W2058197119 hasConceptScore W2058197119C127313418 @default.
• W2058197119 hasConceptScore W2058197119C127413603 @default.
• W2058197119 hasConceptScore W2058197119C142362112 @default.
• W2058197119 hasConceptScore W2058197119C146978453 @default.
• W2058197119 hasConceptScore W2058197119C153294291 @default.
• W2058197119 hasConceptScore W2058197119C19269812 @default.
• W2058197119 hasConceptScore W2058197119C195452092 @default.
• W2058197119 hasConceptScore W2058197119C195886398 @default.
• W2058197119 hasConceptScore W2058197119C197046000 @default.
• W2058197119 hasConceptScore W2058197119C205649164 @default.
• W2058197119 hasConceptScore W2058197119C2777480484 @default.
• W2058197119 hasConceptScore W2058197119C39432304 @default.

• next