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Grant: Discovery Grants Program - Northern Research Supplement

Université du Québec à Rimouski

$14,500.00

Geomagnetic field dynamics and abrupt changes in the Arctic

FY 2012-13

Summary
The geomagnetic field has undergone dramatic changes over the last century. This is best illustrated by changes in the position of the North Magnetic Pole (NMP) and the rapid decline of the dipole field (i.e, the main component of Earth's magnetic field). The NMP, restricted to the Canadian Arctic during historical times, has recently moved into the Arctic Ocean. Direct observations reveal that the migration of the NMP has increased dramatically since the early 1970's from 9 km/yr to 41 km/yr and to almost 60 km/yr in 2003, whereas the annual rate of change in intensity measured at the Resolute Bay geomagnetic observatory has increased from about 10 nT/yr to almost 70 nT/yr over the last 50 years. These spectacular changes lead to the formulation of the following questions: ""Are we in the initial stages of a large-scale geomagnetic change, or even a reversal?"", and if so, ""What are the causes (in Earth's core) and consequences (to Earth's environment) of a large scale geomagnetic change?"" To answer these fundamental questions, the historical record must first be placed into a longer geological context. The long-term goal of this research program is thus to determine the high frequency dynamics of the geomagnetic field during the Late Quaternary in the Arctic with a special emphasis on abrupt changes. This research program will provide the first large-scale study of geomagnetic field dynamics in the Arctic. In addition, by selecting coring sites with very high sediment accumulation rates, the proposed research will investigate geomagnetic field variability at a temporal resolution that is just beginning to be explored, the centennial to millennial timescales. These observations will: 1) enable testing of hypotheses developed from the historical migration of the NMP, 2) yield invaluable data for geodynamo modelling, and 3) place the current dramatic collapse and migration of the NMP into a detailed geological context. Finally, exploring the potential linkages between climate change and geomagnetic field morphology deserves special attention at this time of rapid Arctic climatic change as no current numerical climate model accounts for the possible influence of cosmic rays or the geomagnetic field on climate.
Program
Discovery Grants Program - Northern Research Supplement
Location
Quebec, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data

As published

Application id
316233-2012
Name nom
StOnge, Guillaume
Department département
Sciences de la mer de Rimouski, Institut des
Organization id
58
Institution établissement
Université du Québec à Rimouski
Province en
Québec
Province fr
Québec
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2012
Competition year année de concours
2012
Award amount
14500
Program id
RGPNS
Program name en
Discovery Grants Program - Northern Research Supplement
Program name fr
Porgramme de subventions à la découverte - supplément en recherche nordique
Group en
Discovery grants programs
Group fr
Programmes de subventions à la découverte
Committee code
1025
Committee name en
Northern Research Supplement Program
Committee name fr
Programme de suppléments en recherche nordique
Area of application code
1203
Area of application group en
Advancement of knowledge
Area of application group fr
Avancement des connaissances
Area of application en
Earth sciences
Area of application fr
Sciences de la terre
Research subject code
4303
Research subject group en
Geophysics
Research subject group fr
Géophysique
Research subject en
Paleomagnetism, rock and mineral magnetism
Research subject fr
Paléomagnétisme, magnétisme des roches et minéraux
Partie
1
Nb partie
5
Application title
Geomagnetic field dynamics and abrupt changes in the Arctic
Keyword
NSERC
Application summary
The geomagnetic field has undergone dramatic changes over the last century. This is best illustrated by changes in the position of the North Magnetic Pole (NMP) and the rapid decline of the dipole field (i.e, the main component of Earth's magnetic field). The NMP, restricted to the Canadian Arctic during historical times, has recently moved into the Arctic Ocean. Direct observations reveal that the migration of the NMP has increased dramatically since the early 1970's from 9 km/yr to 41 km/yr and to almost 60 km/yr in 2003, whereas the annual rate of change in intensity measured at the Resolute Bay geomagnetic observatory has increased from about 10 nT/yr to almost 70 nT/yr over the last 50 years. These spectacular changes lead to the formulation of the following questions: ""Are we in the initial stages of a large-scale geomagnetic change, or even a reversal?"", and if so, ""What are the causes (in Earth's core) and consequences (to Earth's environment) of a large scale geomagnetic change?"" To answer these fundamental questions, the historical record must first be placed into a longer geological context. The long-term goal of this research program is thus to determine the high frequency dynamics of the geomagnetic field during the Late Quaternary in the Arctic with a special emphasis on abrupt changes. This research program will provide the first large-scale study of geomagnetic field dynamics in the Arctic. In addition, by selecting coring sites with very high sediment accumulation rates, the proposed research will investigate geomagnetic field variability at a temporal resolution that is just beginning to be explored, the centennial to millennial timescales. These observations will: 1) enable testing of hypotheses developed from the historical migration of the NMP, 2) yield invaluable data for geodynamo modelling, and 3) place the current dramatic collapse and migration of the NMP into a detailed geological context. Finally, exploring the potential linkages between climate change and geomagnetic field morphology deserves special attention at this time of rapid Arctic climatic change as no current numerical climate model accounts for the possible influence of cosmic rays or the geomagnetic field on climate.