His primary areas of study are Holocene, Fluvial, Oceanography, Ice sheet and Geomorphology. His studies deal with areas such as Peat, Coastal erosion, Flood myth and Subsidence as well as Holocene. His study with Fluvial involves better knowledge in Paleontology.
His Paleontology study combines topics from a wide range of disciplines, such as Climate change and Earth science. His Ice core and Climate science study in the realm of Oceanography interacts with subjects such as Greenland Ice Sheet Project, Greenland ice core project and Ice cap climate. He interconnects Arctic ice pack, Ice age, Forebulge and Sea level in the investigation of issues within Ice sheet.
His main research concerns Holocene, Oceanography, Sea level, Geomorphology and Sediment. Holocene is a subfield of Paleontology that Torbjörn E. Törnqvist tackles. His work on Sea level rise and Continental shelf as part of general Oceanography research is frequently linked to Mississippi delta, bridging the gap between disciplines.
His Post-glacial rebound study in the realm of Sea level interacts with subjects such as Event. His work deals with themes such as Sedimentary rock and Stratigraphy, which intersect with Geomorphology. His work investigates the relationship between Sediment and topics such as Hydrology that intersect with problems in Crevasse splay.
Torbjörn E. Törnqvist spends much of his time researching Sediment, Hydrology, Physical geography, River delta and Geomorphology. As a member of one scientific family, Torbjörn E. Törnqvist mostly works in the field of Sediment, focusing on Flooding and, on occasion, Subsidence, Post-glacial rebound, Extraction, Tectonics and Lead. His Hydrology study incorporates themes from Radiocarbon dating and Levee.
The Physical geography study combines topics in areas such as Climate change, Subsidence, Holocene and Progradation. His Holocene research is multidisciplinary, relying on both Shore, Sea level, Ice sheet, Landform and Coastal restoration. His Sea level study is associated with Oceanography.
His primary scientific interests are in Sediment, Physical geography, River delta, Climate change and Holocene. His Sediment research is multidisciplinary, incorporating perspectives in Elevation, Tide gauge, Flooding and Subsidence. His Physical geography research integrates issues from Spatial ecology, Mediterranean climate, Last Glacial Maximum and Ice sheet.
His River delta research incorporates Hydrology, Geomorphology, Alluvium, Estuary and Fluvial. Torbjörn E. Törnqvist combines subjects such as Dominance, Sea level and Physical oceanography with his study of Climate change. Torbjörn E. Törnqvist merges many fields, such as Holocene and Mississippi delta, in his writings.
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Fluvial responses to climate and sea‐level change: a review and look forward
Michael D. Blum;Torbjörn E. Törnqvist.
Mississippi Delta subsidence primarily caused by compaction of Holocene strata
Torbjörn E. Törnqvist;Davin J. Wallace;Davin J. Wallace;Joep E. A. Storms;Joep E. A. Storms;Jakob Wallinga;Jakob Wallinga.
Nature Geoscience (2008)
Accurate Dating of Organic Deposits by AMS 14C Measurement of Macrofossils
Torbjörn E. Törnqvist;Arie F. M. de Jong;Wilma A. Oosterbaan;Klaas Van Der Borg.
Deciphering Holocene sea-level history on the U.S. Gulf Coast: A high-resolution record from the Mississippi Delta
Torbjörn E. Törnqvist;Juan L. González;Lee A. Newsom;Klaas van der Borg.
Geological Society of America Bulletin (2004)
Holocene Alternation of Meandering and Anastomosing Fluvial Systems in the Rhine-Meuse Delta (Central Netherlands) Controlled by Sea-Level Rise and Subsoil Erodibility
Torbjorn E. Tornqvist.
Journal of Sedimentary Research (1993)
Spatial variability of late Holocene and 20th century sea-level rise along the Atlantic coast of the United States
Simon E. Engelhart;Benjamin P. Horton;Bruce C. Douglas;W. Richard Peltier.
A Revised Chronology for Mississippi River Subdeltas
Torbjörn E. Törnqvist;Tristram R. Kidder;Whitney J. Autin;Klaas van der Borg.
Middle and late Holocene avulsion history of the River Rhine (Rhine-Meuse delta, Netherlands)
Torbjörn E. Törnqvist.
Spatial variation of overbank aggradation rate and its influence on avulsion frequency
Torbjörn E. Törnqvist;John S. Bridge.
Testing optically stimulated luminescence dating of sand-sized quartz and feldspar from fluvial deposits
J. Wallinga;J. Wallinga;J. Wallinga;A.S. Murray;G.A.T. Duller;T.E. Törnqvist.
Earth and Planetary Science Letters (2001)
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