FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2169190286> ?p ?o ?g. }

• W2169190286 endingPage "849" @default.
• W2169190286 startingPage "835" @default.
• W2169190286 abstract "Aim Greenhouse‐induced warming and resulting shifts in climatic zones may exceed the migration capabilities of some species. We used fourteen combinations of General Circulation Models (GCMs) and Global Vegetation Models (GVMs) to investigate possible migration rates required under CO 2 ‐doubled climatic forcing. Location Global. Methods Migration distances were calculated between grid cells of future biome type x and nearest same‐biome‐type cells in the current climate. In `base‐case' calculations, we assumed that 2 × CO 2 climate forcing would occur in 100 years, we used ten biome types and we measured migration distances as straight‐line distances ignoring water barriers and human development. In sensitivity analyses, we investigated different time periods of 2 × CO 2 climate forcing, more narrowly defined biomes and barriers because of water bodies and human development. Results In the base‐case calculations, average migration rates varied significantly according to the GVM used (BIOME3 vs. MAPSS), the age of the GCM (older‐ vs. newer‐generation GCMs), and whether or not GCMs included sulphate cooling or CO 2 fertilization effects. However, high migration rates (≥ 1000 m year −1 ) were relatively common in all models, consisting on average of 17% grid cells for BIOME3 and 21% for MAPSS. Migration rates were much higher in boreal and temperate biomes than in tropical biomes. Doubling of the time period of 2 × CO 2 forcing reduced these areas of high migration rates to c . 12% of grid cells for both BIOME3 and MAPSS. However, to obtain migration rates in the Boreal biome that were similar in magnitude to those observed for spruce when it followed the retreating North American Glacier, a radical increase in the period of warming was required, from 100 to >1000 years. A reduction in biome area by an order of magnitude increased migration rates by one to three orders of magnitude, depending on the GVM. Large water bodies and human development had regionally important effects in increasing migration rates. Main conclusions In conclusion, evidence from coupled GCMs and GVMs suggests that global warming may require migration rates much faster than those observed during post‐glacial times and hence has the potential to reduce biodiversity by selecting for highly mobile and opportunistic species. Several poorly understood factors that are expected to influence the magnitude of any such reduction are discussed, including intrinsic migrational capabilities, barriers to migration, the role of outlier populations in increasing migration rates, the role of climate in setting range limits and variation in species range sizes." @default.
• W2169190286 created "2016-06-24" @default.
• W2169190286 creator A5019870560 @default.
• W2169190286 creator A5048591997 @default.
• W2169190286 creator A5080011358 @default.
• W2169190286 creator A5090176695 @default.
• W2169190286 date "2002-07-01" @default.
• W2169190286 modified "2023-10-13" @default.
• W2169190286 title "Estimated migration rates under scenarios of global climate change" @default.
• W2169190286 cites W103534397 @default.
• W2169190286 cites W1519918296 @default.
• W2169190286 cites W1563720491 @default.
• W2169190286 cites W1589626869 @default.
• W2169190286 cites W1597373514 @default.
• W2169190286 cites W170688703 @default.
• W2169190286 cites W1938225006 @default.
• W2169190286 cites W1976786267 @default.
• W2169190286 cites W1988618524 @default.
• W2169190286 cites W1993644529 @default.
• W2169190286 cites W1995018497 @default.
• W2169190286 cites W2013830328 @default.
• W2169190286 cites W2019975015 @default.
• W2169190286 cites W2044410193 @default.
• W2169190286 cites W2045411870 @default.
• W2169190286 cites W2047384175 @default.
• W2169190286 cites W2047751191 @default.
• W2169190286 cites W2052558531 @default.
• W2169190286 cites W2065895599 @default.
• W2169190286 cites W2072344215 @default.
• W2169190286 cites W2074298000 @default.
• W2169190286 cites W2086075858 @default.
• W2169190286 cites W2088491606 @default.
• W2169190286 cites W2098323790 @default.
• W2169190286 cites W2105247575 @default.
• W2169190286 cites W2113053672 @default.
• W2169190286 cites W2113068240 @default.
• W2169190286 cites W2113890242 @default.
• W2169190286 cites W2124991269 @default.
• W2169190286 cites W2127559745 @default.
• W2169190286 cites W2135735088 @default.
• W2169190286 cites W2138077181 @default.
• W2169190286 cites W2150231777 @default.
• W2169190286 cites W2152865972 @default.
• W2169190286 cites W2163326970 @default.
• W2169190286 cites W2179879290 @default.
• W2169190286 cites W2319372310 @default.
• W2169190286 cites W2319754122 @default.
• W2169190286 cites W2329576516 @default.
• W2169190286 cites W2371985437 @default.
• W2169190286 cites W2775445625 @default.
• W2169190286 cites W2795815544 @default.
• W2169190286 cites W302391044 @default.
• W2169190286 cites W4245212515 @default.
• W2169190286 cites W4249149877 @default.
• W2169190286 cites W4367727136 @default.
• W2169190286 cites W86596393 @default.
• W2169190286 doi "https://doi.org/10.1046/j.1365-2699.2002.00702.x" @default.
• W2169190286 hasPublicationYear "2002" @default.
• W2169190286 type Work @default.
• W2169190286 sameAs 2169190286 @default.
• W2169190286 citedByCount "311" @default.
• W2169190286 countsByYear W21691902862012 @default.
• W2169190286 countsByYear W21691902862013 @default.
• W2169190286 countsByYear W21691902862014 @default.
• W2169190286 countsByYear W21691902862015 @default.
• W2169190286 countsByYear W21691902862016 @default.
• W2169190286 countsByYear W21691902862017 @default.
• W2169190286 countsByYear W21691902862018 @default.
• W2169190286 countsByYear W21691902862019 @default.
• W2169190286 countsByYear W21691902862020 @default.
• W2169190286 countsByYear W21691902862021 @default.
• W2169190286 countsByYear W21691902862022 @default.
• W2169190286 countsByYear W21691902862023 @default.
• W2169190286 crossrefType "journal-article" @default.
• W2169190286 hasAuthorship W2169190286A5019870560 @default.
• W2169190286 hasAuthorship W2169190286A5048591997 @default.
• W2169190286 hasAuthorship W2169190286A5080011358 @default.
• W2169190286 hasAuthorship W2169190286A5090176695 @default.
• W2169190286 hasConcept C100537666 @default.
• W2169190286 hasConcept C100970517 @default.
• W2169190286 hasConcept C110872660 @default.
• W2169190286 hasConcept C115343472 @default.
• W2169190286 hasConcept C122523270 @default.
• W2169190286 hasConcept C127313418 @default.
• W2169190286 hasConcept C132651083 @default.
• W2169190286 hasConcept C13280743 @default.
• W2169190286 hasConcept C141452985 @default.
• W2169190286 hasConcept C168754636 @default.
• W2169190286 hasConcept C18903297 @default.
• W2169190286 hasConcept C197115733 @default.
• W2169190286 hasConcept C205649164 @default.
• W2169190286 hasConcept C39432304 @default.
• W2169190286 hasConcept C49204034 @default.
• W2169190286 hasConcept C81461190 @default.
• W2169190286 hasConcept C86803240 @default.
• W2169190286 hasConcept C89920630 @default.
• W2169190286 hasConcept C91586092 @default.
• W2169190286 hasConcept C99578197 @default.

• next