FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1963669976> ?p ?o ?g. }

• W1963669976 endingPage "1211" @default.
• W1963669976 startingPage "1203" @default.
• W1963669976 abstract "Abstract. Atmospheric warming over the Greenland Ice Sheet during the last 2 decades has increased the amount of surface meltwater production, resulting in the migration of melt and percolation regimes to higher altitudes and an increase in the amount of ice content from refrozen meltwater found in the firn above the superimposed ice zone. Here we present field and airborne radar observations of buried ice layers within the near-surface (0–20 m) firn in western Greenland, obtained from campaigns between 1998 and 2014. We find a sharp increase in firn-ice content in the form of thick widespread layers in the percolation zone, which decreases the capacity of the firn to store meltwater. The estimated total annual ice content retained in the near-surface firn in areas with positive surface mass balance west of the ice divide in Greenland reached a maximum of 74 ± 25 Gt in 2012, compared to the 1958–1999 average of 13 ± 2 Gt, while the percolation zone area more than doubled between 2003 and 2012. Increased melt and column densification resulted in surface lowering averaging −0.80 ± 0.39 m yr−1 between 1800 and 2800 m in the accumulation zone of western Greenland. Since 2007, modeled annual melt and refreezing rates in the percolation zone at elevations below 2100 m surpass the annual snowfall from the previous year, implying that mass gain in the region is retained after melt in the form of refrozen meltwater. If current melt trends over high elevation regions continue, subsequent changes in firn structure will have implications for the hydrology of the ice sheet and related abrupt seasonal densification could become increasingly significant for altimetry-derived ice sheet mass balance estimates." @default.
• W1963669976 created "2016-06-24" @default.
• W1963669976 creator A5004263989 @default.
• W1963669976 creator A5025794003 @default.
• W1963669976 creator A5032253957 @default.
• W1963669976 creator A5042973613 @default.
• W1963669976 creator A5053385922 @default.
• W1963669976 creator A5068237537 @default.
• W1963669976 creator A5068282620 @default.
• W1963669976 creator A5068628691 @default.
• W1963669976 creator A5088517608 @default.
• W1963669976 date "2015-06-11" @default.
• W1963669976 modified "2023-10-16" @default.
• W1963669976 title "Changes in the firn structure of the western Greenland Ice Sheet caused by recent warming" @default.
• W1963669976 cites W1893479695 @default.
• W1963669976 cites W1969320838 @default.
• W1963669976 cites W1975369353 @default.
• W1963669976 cites W1976860445 @default.
• W1963669976 cites W1983134663 @default.
• W1963669976 cites W1983646865 @default.
• W1963669976 cites W1988571084 @default.
• W1963669976 cites W1994138832 @default.
• W1963669976 cites W2003446785 @default.
• W1963669976 cites W2004902078 @default.
• W1963669976 cites W2012556732 @default.
• W1963669976 cites W2027731203 @default.
• W1963669976 cites W2037250748 @default.
• W1963669976 cites W2037864830 @default.
• W1963669976 cites W2043278879 @default.
• W1963669976 cites W2046175251 @default.
• W1963669976 cites W2062866220 @default.
• W1963669976 cites W2062940877 @default.
• W1963669976 cites W2069842022 @default.
• W1963669976 cites W2090357101 @default.
• W1963669976 cites W2092683021 @default.
• W1963669976 cites W2092934455 @default.
• W1963669976 cites W2113149411 @default.
• W1963669976 cites W2117558319 @default.
• W1963669976 cites W2126271194 @default.
• W1963669976 cites W2128112636 @default.
• W1963669976 cites W2131901831 @default.
• W1963669976 cites W2140534161 @default.
• W1963669976 cites W2143671171 @default.
• W1963669976 cites W2152415573 @default.
• W1963669976 cites W2161306464 @default.
• W1963669976 cites W2164147693 @default.
• W1963669976 doi "https://doi.org/10.5194/tc-9-1203-2015" @default.
• W1963669976 hasPublicationYear "2015" @default.
• W1963669976 type Work @default.
• W1963669976 sameAs 1963669976 @default.
• W1963669976 citedByCount "42" @default.
• W1963669976 countsByYear W19636699762016 @default.
• W1963669976 countsByYear W19636699762017 @default.
• W1963669976 countsByYear W19636699762018 @default.
• W1963669976 countsByYear W19636699762019 @default.
• W1963669976 countsByYear W19636699762020 @default.
• W1963669976 countsByYear W19636699762021 @default.
• W1963669976 countsByYear W19636699762022 @default.
• W1963669976 countsByYear W19636699762023 @default.
• W1963669976 crossrefType "journal-article" @default.
• W1963669976 hasAuthorship W1963669976A5004263989 @default.
• W1963669976 hasAuthorship W1963669976A5025794003 @default.
• W1963669976 hasAuthorship W1963669976A5032253957 @default.
• W1963669976 hasAuthorship W1963669976A5042973613 @default.
• W1963669976 hasAuthorship W1963669976A5053385922 @default.
• W1963669976 hasAuthorship W1963669976A5068237537 @default.
• W1963669976 hasAuthorship W1963669976A5068282620 @default.
• W1963669976 hasAuthorship W1963669976A5068628691 @default.
• W1963669976 hasAuthorship W1963669976A5088517608 @default.
• W1963669976 hasBestOaLocation W19636699761 @default.
• W1963669976 hasConcept C100970517 @default.
• W1963669976 hasConcept C104730834 @default.
• W1963669976 hasConcept C114793014 @default.
• W1963669976 hasConcept C123750103 @default.
• W1963669976 hasConcept C127313418 @default.
• W1963669976 hasConcept C136894858 @default.
• W1963669976 hasConcept C169760540 @default.
• W1963669976 hasConcept C193091731 @default.
• W1963669976 hasConcept C197046000 @default.
• W1963669976 hasConcept C197435368 @default.
• W1963669976 hasConcept C205325660 @default.
• W1963669976 hasConcept C205649164 @default.
• W1963669976 hasConcept C207318512 @default.
• W1963669976 hasConcept C2780021526 @default.
• W1963669976 hasConcept C2780457167 @default.
• W1963669976 hasConcept C49204034 @default.
• W1963669976 hasConcept C81820708 @default.
• W1963669976 hasConcept C86803240 @default.
• W1963669976 hasConcept C91586092 @default.
• W1963669976 hasConceptScore W1963669976C100970517 @default.
• W1963669976 hasConceptScore W1963669976C104730834 @default.
• W1963669976 hasConceptScore W1963669976C114793014 @default.
• W1963669976 hasConceptScore W1963669976C123750103 @default.
• W1963669976 hasConceptScore W1963669976C127313418 @default.
• W1963669976 hasConceptScore W1963669976C136894858 @default.
• W1963669976 hasConceptScore W1963669976C169760540 @default.
• W1963669976 hasConceptScore W1963669976C193091731 @default.
• W1963669976 hasConceptScore W1963669976C197046000 @default.

• next