FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W258914707> ?p ?o ?g. }

• W258914707 endingPage "149" @default.
• W258914707 startingPage "135" @default.
• W258914707 abstract "Abstract The formation of superimposed ice in the accumulation area of sub-polar glaciers plays an important role in the heat and mass balance of the glaciers. In order to study the process of superimposed ice formation in detail, field observations were conducted on McCall Glacier, a sub-polar glacier in Arctic Alaska. It was found that the approximate thickness of superimposed ice formed in a whole summer was 20 cm in the upper region and 30—40 cm in the lower region of the accumulation area of the glacier. This difference in thickness may be attributed to the difference in the temperature of the underlying ice and the rate of supply of melt water. The ratio of the amount of superimposed ice formed in the accumulation area from May to July in 1972 to the total amount of melt was determined. Approximately 50% of the total melt water was discharged from the glacier as run-off water, and the remainder contributed to the formation of superimposed ice. An experimental study on the artificial formation of superimposed ice was conducted in the cold laboratory to obtain the ratio of superimposed ice, that of run-off water, and that of free water suspended between snow grains, to the total amount of melt water produced in the snow. The ratios obtained in the laboratory experiment agree fairly well with those derived from the observational data on McCall Glacier. Numerical calculations were conducted to examine the relationship between the growth rate of superimposed ice, the rale of snow melting, the rate of discharge of excess melt-water, and the temperature of the underlying ice. Calculations were made in reference to both the laboratory experiment and the field observations on McCall Glacier. It was found that the predominant factors controlling the growth rate or the total amount of superimposed ice in a sub-polar glacier are the rate of supply of melt water to the snow-ice interface and the initial temperature distribution in the underlying ice. By using the present calculation, it may be possible to estimate the growth rate, the total amount of superimposed ice, and the ratio of superimposed ice to the total amount of melting in the accumulation area of any sub-polar glacier, if observational data on the initial temperature distribution in ice and the rate of snow melting at the snow surface are available." @default.
• W258914707 created "2016-06-24" @default.
• W258914707 creator A5014311269 @default.
• W258914707 creator A5018301330 @default.
• W258914707 creator A5059383916 @default.
• W258914707 creator A5061405993 @default.
• W258914707 date "1976-01-01" @default.
• W258914707 modified "2023-09-23" @default.
• W258914707 title "Field Observations and Experimental and Theoretical Studies on the Superimposed Ice of McCall Glacier, Alaska" @default.
• W258914707 cites W120948415 @default.
• W258914707 cites W2586675388 @default.
• W258914707 cites W278133456 @default.
• W258914707 cites W41576189 @default.
• W258914707 cites W4239274436 @default.
• W258914707 doi "https://doi.org/10.1017/s0022143000031488" @default.
• W258914707 hasPublicationYear "1976" @default.
• W258914707 type Work @default.
• W258914707 sameAs 258914707 @default.
• W258914707 citedByCount "44" @default.
• W258914707 countsByYear W2589147072012 @default.
• W258914707 countsByYear W2589147072013 @default.
• W258914707 countsByYear W2589147072018 @default.
• W258914707 countsByYear W2589147072019 @default.
• W258914707 crossrefType "journal-article" @default.
• W258914707 hasAuthorship W258914707A5014311269 @default.
• W258914707 hasAuthorship W258914707A5018301330 @default.
• W258914707 hasAuthorship W258914707A5059383916 @default.
• W258914707 hasAuthorship W258914707A5061405993 @default.
• W258914707 hasBestOaLocation W2589147071 @default.
• W258914707 hasConcept C100834320 @default.
• W258914707 hasConcept C104932425 @default.
• W258914707 hasConcept C111368507 @default.
• W258914707 hasConcept C114793014 @default.
• W258914707 hasConcept C121332964 @default.
• W258914707 hasConcept C127313418 @default.
• W258914707 hasConcept C1276947 @default.
• W258914707 hasConcept C136894858 @default.
• W258914707 hasConcept C161798024 @default.
• W258914707 hasConcept C16335420 @default.
• W258914707 hasConcept C171289182 @default.
• W258914707 hasConcept C193091731 @default.
• W258914707 hasConcept C197046000 @default.
• W258914707 hasConcept C197435368 @default.
• W258914707 hasConcept C29705727 @default.
• W258914707 hasConcept C49204034 @default.
• W258914707 hasConcept C518008717 @default.
• W258914707 hasConcept C65748596 @default.
• W258914707 hasConcept C81820708 @default.
• W258914707 hasConceptScore W258914707C100834320 @default.
• W258914707 hasConceptScore W258914707C104932425 @default.
• W258914707 hasConceptScore W258914707C111368507 @default.
• W258914707 hasConceptScore W258914707C114793014 @default.
• W258914707 hasConceptScore W258914707C121332964 @default.
• W258914707 hasConceptScore W258914707C127313418 @default.
• W258914707 hasConceptScore W258914707C1276947 @default.
• W258914707 hasConceptScore W258914707C136894858 @default.
• W258914707 hasConceptScore W258914707C161798024 @default.
• W258914707 hasConceptScore W258914707C16335420 @default.
• W258914707 hasConceptScore W258914707C171289182 @default.
• W258914707 hasConceptScore W258914707C193091731 @default.
• W258914707 hasConceptScore W258914707C197046000 @default.
• W258914707 hasConceptScore W258914707C197435368 @default.
• W258914707 hasConceptScore W258914707C29705727 @default.
• W258914707 hasConceptScore W258914707C49204034 @default.
• W258914707 hasConceptScore W258914707C518008717 @default.
• W258914707 hasConceptScore W258914707C65748596 @default.
• W258914707 hasConceptScore W258914707C81820708 @default.
• W258914707 hasIssue "74" @default.
• W258914707 hasLocation W2589147071 @default.
• W258914707 hasOpenAccess W258914707 @default.
• W258914707 hasPrimaryLocation W2589147071 @default.
• W258914707 hasRelatedWork W1978756959 @default.
• W258914707 hasRelatedWork W1991176747 @default.
• W258914707 hasRelatedWork W2084381294 @default.
• W258914707 hasRelatedWork W2090030785 @default.
• W258914707 hasRelatedWork W2147454773 @default.
• W258914707 hasRelatedWork W2177582843 @default.
• W258914707 hasRelatedWork W2345934419 @default.
• W258914707 hasRelatedWork W2601504434 @default.
• W258914707 hasRelatedWork W3097216428 @default.
• W258914707 hasRelatedWork W4377081327 @default.
• W258914707 hasVolume "16" @default.
• W258914707 isParatext "false" @default.
• W258914707 isRetracted "false" @default.
• W258914707 magId "258914707" @default.
• W258914707 workType "article" @default.