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The Importance of Understanding the Last Glacial Maximum for Climate Change
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Long-term carbon storage shifts in high-latitude peatlands with paleoclimate cha...
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Long-term carbon storage shifts in high-latitude peatlands with paleoclimate cha...
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Age determinations on peat profile Pur-Taz
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Postglacial migration history of lodgepole pine near Yakutat, Alaska
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Modern Pollen Rain and Vegetational History of the Malaspina Glacier District, A...
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Oxygen Isotopes in Fresh Water Biogenic Opal: Northeastern US Alleroed-Younger D...
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Late-Glacial to Early Holocene Climate Changes from a Central Appalachians Polle...
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Late-Glacial to Early Holocene Climate Changes from a Central Appalachian Pollen...
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Fish Scale Evidence for Rapid Post Glacial Colonization of an Atlantic Coastal P...
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Late-glacial vegetational, tephra, and climatic history of southwestern Kodiak I...
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Extent and Timing of the Last Glacial Maximum in Southwestern Alaska
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Editorial: North Pacific Environment and Paleoclimate from the Late Pleistocene...
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A Deglacial and Holocene Record of Climate Variability in South-Central Alaska f...
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Long-Term Arctic Peatland Dynamics, Vegetation and Climate History of the Pur-Ta...
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Long‐term Arctic peatland dynamics, vegetation and climate history of the Pur‐Ta...
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Holocene Vegetation, Climate, and Carbon History on Western Kodiak Island, Alask...
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Holocene Vegetation, Climate, and Carbon History on Western Kodiak Island, Alask...
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Holocene Ecohydrological Variability on the East Coast of Kamchatka
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Holocene Ecohydrological Variability on the East Coast of Kamchatka
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Meteorology and Climatology
Atmosphere
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[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
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Climatic changes--Effect of human beings on
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