FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2168060352> ?p ?o ?g. }

• W2168060352 endingPage "305" @default.
• W2168060352 startingPage "291" @default.
• W2168060352 abstract "Abstract There are many lakes of widely varying morphometry in northern latitudes. For this study region, in the central Mackenzie River valley of western Canada, lakes make up 37% of the landscape. The nonlake components of the landscape are divided into uplands (55%) and wetlands (8%). With such abundance, lakes are important features that can influence the regional climate. This paper examines the role of lakes in the regional surface energy and water balance and evaluates the links to the frequency–size distribution of lakes. The primary purpose is to examine how the surface energy balance may influence regional climate and weather. Lakes are characterized by both the magnitude and temporal behavior of their surface energy balances during the ice-free period. The impacts of combinations of various-size lakes and land–lake distributions on regional energy balances and evaporation cycles are presented. Net radiation is substantially greater over all water-dominated surfaces compared with uplands. The seasonal heat storage increases with lake size. Medium and large lakes are slow to warm in summer. Their large cumulative heat storage, near summer’s end, fuels large convective heat fluxes in fall and early winter. The evaporation season for upland, wetland, and small, medium, and large lakes lasts for 19, 21, 22, 24, and 30 weeks, respectively. The regional effects of combinations of surface types are derived. The region is initially treated as comprising uplands only. The influences of wetland, small, medium, and large lakes are added sequentially, to build up to the energy budget of the actual landscape. The addition of lakes increases the regional net radiation, the maximum regional subsurface heat storage, and evaporation substantially. Evaporation decreases slightly in the first half of the season but experiences a large enhancement in the second half. The sensible heat flux is reduced substantially in the first half of the season, but changes little in the second half. For energy budget modeling the representation of lake size is important. Net radiation is fairly independent of size. An equal area of medium and large lakes, compared with small lakes, yields substantially larger latent heat fluxes and lesser sensible heat fluxes. Lake size also creates large differences in regional flux magnitudes, especially in the spring and fall periods." @default.
• W2168060352 created "2016-06-24" @default.
• W2168060352 creator A5000191283 @default.
• W2168060352 creator A5015767147 @default.
• W2168060352 creator A5051239673 @default.
• W2168060352 creator A5053640900 @default.
• W2168060352 creator A5064412993 @default.
• W2168060352 creator A5069727604 @default.
• W2168060352 creator A5085615058 @default.
• W2168060352 creator A5090026664 @default.
• W2168060352 date "2005-06-01" @default.
• W2168060352 modified "2023-10-10" @default.
• W2168060352 title "The Role of Northern Lakes in a Regional Energy Balance" @default.
• W2168060352 cites W1510808113 @default.
• W2168060352 cites W1975911636 @default.
• W2168060352 cites W1984822089 @default.
• W2168060352 cites W2011466318 @default.
• W2168060352 cites W2045866576 @default.
• W2168060352 cites W2050531929 @default.
• W2168060352 cites W2051310849 @default.
• W2168060352 cites W2053801545 @default.
• W2168060352 cites W2059014173 @default.
• W2168060352 cites W2082787430 @default.
• W2168060352 cites W2086085022 @default.
• W2168060352 cites W2099882751 @default.
• W2168060352 cites W2136996194 @default.
• W2168060352 cites W2159923592 @default.
• W2168060352 cites W2173934470 @default.
• W2168060352 cites W2174409238 @default.
• W2168060352 cites W2174922262 @default.
• W2168060352 cites W2180812781 @default.
• W2168060352 cites W2181040308 @default.
• W2168060352 cites W2340977953 @default.
• W2168060352 cites W2416838637 @default.
• W2168060352 doi "https://doi.org/10.1175/jhm421.1" @default.
• W2168060352 hasPublicationYear "2005" @default.
• W2168060352 type Work @default.
• W2168060352 sameAs 2168060352 @default.
• W2168060352 citedByCount "133" @default.
• W2168060352 countsByYear W21680603522012 @default.
• W2168060352 countsByYear W21680603522013 @default.
• W2168060352 countsByYear W21680603522014 @default.
• W2168060352 countsByYear W21680603522015 @default.
• W2168060352 countsByYear W21680603522016 @default.
• W2168060352 countsByYear W21680603522017 @default.
• W2168060352 countsByYear W21680603522018 @default.
• W2168060352 countsByYear W21680603522019 @default.
• W2168060352 countsByYear W21680603522020 @default.
• W2168060352 countsByYear W21680603522021 @default.
• W2168060352 countsByYear W21680603522022 @default.
• W2168060352 countsByYear W21680603522023 @default.
• W2168060352 crossrefType "journal-article" @default.
• W2168060352 hasAuthorship W2168060352A5000191283 @default.
• W2168060352 hasAuthorship W2168060352A5015767147 @default.
• W2168060352 hasAuthorship W2168060352A5051239673 @default.
• W2168060352 hasAuthorship W2168060352A5053640900 @default.
• W2168060352 hasAuthorship W2168060352A5064412993 @default.
• W2168060352 hasAuthorship W2168060352A5069727604 @default.
• W2168060352 hasAuthorship W2168060352A5085615058 @default.
• W2168060352 hasAuthorship W2168060352A5090026664 @default.
• W2168060352 hasBestOaLocation W21680603521 @default.
• W2168060352 hasConcept C100970517 @default.
• W2168060352 hasConcept C111368507 @default.
• W2168060352 hasConcept C122523270 @default.
• W2168060352 hasConcept C127313418 @default.
• W2168060352 hasConcept C132651083 @default.
• W2168060352 hasConcept C13280743 @default.
• W2168060352 hasConcept C153294291 @default.
• W2168060352 hasConcept C187320778 @default.
• W2168060352 hasConcept C18903297 @default.
• W2168060352 hasConcept C205649164 @default.
• W2168060352 hasConcept C2777423268 @default.
• W2168060352 hasConcept C39432304 @default.
• W2168060352 hasConcept C61441594 @default.
• W2168060352 hasConcept C66465714 @default.
• W2168060352 hasConcept C67715294 @default.
• W2168060352 hasConcept C76886044 @default.
• W2168060352 hasConcept C86803240 @default.
• W2168060352 hasConceptScore W2168060352C100970517 @default.
• W2168060352 hasConceptScore W2168060352C111368507 @default.
• W2168060352 hasConceptScore W2168060352C122523270 @default.
• W2168060352 hasConceptScore W2168060352C127313418 @default.
• W2168060352 hasConceptScore W2168060352C132651083 @default.
• W2168060352 hasConceptScore W2168060352C13280743 @default.
• W2168060352 hasConceptScore W2168060352C153294291 @default.
• W2168060352 hasConceptScore W2168060352C187320778 @default.
• W2168060352 hasConceptScore W2168060352C18903297 @default.
• W2168060352 hasConceptScore W2168060352C205649164 @default.
• W2168060352 hasConceptScore W2168060352C2777423268 @default.
• W2168060352 hasConceptScore W2168060352C39432304 @default.
• W2168060352 hasConceptScore W2168060352C61441594 @default.
• W2168060352 hasConceptScore W2168060352C66465714 @default.
• W2168060352 hasConceptScore W2168060352C67715294 @default.
• W2168060352 hasConceptScore W2168060352C76886044 @default.
• W2168060352 hasConceptScore W2168060352C86803240 @default.
• W2168060352 hasIssue "3" @default.
• W2168060352 hasLocation W21680603521 @default.
• W2168060352 hasOpenAccess W2168060352 @default.

• next