Troels Aagaard

ORCID: 0000-0002-7397-8232
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About
Contact & Profiles
Research Areas
  • Coastal and Marine Dynamics
  • Coastal wetland ecosystem dynamics
  • Geological formations and processes
  • Aeolian processes and effects
  • Ocean Waves and Remote Sensing
  • Tropical and Extratropical Cyclones Research
  • Geology and Paleoclimatology Research
  • Methane Hydrates and Related Phenomena
  • Marine and environmental studies
  • Maritime and Coastal Archaeology
  • Geological Modeling and Analysis
  • Soil erosion and sediment transport
  • Underwater Acoustics Research
  • Hydrology and Sediment Transport Processes
  • Aquatic and Environmental Studies
  • Geophysics and Gravity Measurements
  • Cardiovascular and exercise physiology
  • Sports Performance and Training
  • Wave and Wind Energy Systems
  • Income, Poverty, and Inequality
  • Anomaly Detection Techniques and Applications
  • Oceanographic and Atmospheric Processes
  • Time Series Analysis and Forecasting
  • Geomagnetism and Paleomagnetism Studies
  • Neural Networks and Applications

Geocenter Denmark
2007-2021

University of Copenhagen
2012-2021

Danish Geodata Agency
2021

IT University of Copenhagen
2020

The University of Sydney
2013

The Scarborough Hospital
1994-1995

University of Toronto
1994-1995

V. B. Sochava Institute of Geography
1988

Geographical Institute
1985

The Volta River delta developed as an asymmetric lobe in a tectonic offset on the coast of Ghana. comprises large curvilinear spit that widens its central portion due to adjunction successive sandy beach ridges. appearance distinct spit, lieu continuous barrier from present mouth Bight Benin coast, may be outgrowth natural change location Volta. marks segmentation unique sand drift cell hitherto prevailed this bight coast. Spit growth has been accompanied by wave erosion over last century...

10.2989/16085914.2015.1115751 article EN African Journal of Aquatic Science 2016-01-28

Abstract Many beaches have been built by an onshore supply of sand from the shoreface, and future long‐term coastal evolution critically depends on cross‐shore sediment exchange between upper lower shorefaces. Even so, remains poorly known in quantitative terms this reduces confidence predictions shoreline change. In paper, field measurements suspended load transport shoreface are used to derive a model for at large spatial temporal scales. Data collection took place five different sites...

10.1002/2013jf003041 article EN Journal of Geophysical Research Earth Surface 2014-03-28

Abstract This study presents a detailed reconstruction of the sedimentary effects Holocene sea‐level rise on modern coastal barrier system. Increasing concern over evolution systems due to future accelerated rates calls for better understanding response changes. The complex and sequence stratigraphic framework investigated system is reconstructed using facies analysis, high‐resolution optically stimulated luminescence radiocarbon dating. During formation starting 8 7 ka rapid relative...

10.1111/sed.12167 article EN Sedimentology 2014-10-03

1. The present study examined how uptake of lactate and H+ in resting muscle is affected by blood flow, arterial concentration metabolism. 2. Six males subjects performed intermittent arm exercise two separate 32 min periods (Part I Part II) one subsequent 20 period which leg knee‐extensor was also III). at various intensities order to obtain different steady‐state concentrations. In the inactive leg, femoral venous flow (draining about 7.7 kg muscles) measured collected frequently. Biopsies...

10.1113/jphysiol.1995.sp020960 article EN The Journal of Physiology 1995-10-01

Detailed hydrodynamic and morphological data are presented from a field deployment spanning 2 days (four tide cycles). The include bed-elevation changes measured at each low continuous records of water-surface elevation, cross-shore long-shore current velocities, suspended sediment concentrations all within 20 cm the bed. During deployment, an intertidal bar migrated onshore infilled runnel on its landward side. depth this was initially 0.6 m. migration bar, significant wave height in deep...

10.2112/04-0214.1 article EN Journal of Coastal Research 2006-03-01

Most studies of late H olocene sea‐level changes generally assume stable tectonic conditions. However, unrecognized neotectonic ‘noise’, even the small rates passive continental margins, can severely distort reconstructions olocene. The detailed curve proposed here is reconstructed by identification an area ( L æsø archipelago in K attegat S ea) where level and other kinds ‘background noise’ be precisely quantified advanced i DAR techniques. We show that absolute (‘eustatic’) sea has risen...

10.1111/j.1502-3885.2011.00229.x article EN Boreas 2011-10-03
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