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author = "Otterå, Odd Helge"

Found 20 documents, displaying page 2 of 2

Arctic/Atlantic exchanges via the Subpolar Gyre

Description : In the present study we investigate the decadal variability in the strength and shape of the Subpolar Gyre (SPG) in a 600-year pre-industrial simulation using the Bergen Climate Model. The atmospheric influence on the SPG strength is reflected in the variability of Labrador Sea Water (LSW), which is...
Repository : Bergen Open Research Archive (BORA) - UiB
Language(s) : English

The sensitivity of the present-day Atlantic meridional overturning circulation to freshwater forcing

Description : Mounting evidence indicates that the Atlantic Meridional Overturning Circulation (AMOC) was strongly reduced during cold climate episodes in the past, possible due to freshwater influx from glacial melting. It is also expected that the freshwater input to high northern latitudes will increase as hum...
Repository : NORA (Norwegian Open Research Archives)
Language(s) : English

The sensitivity of the present-day Atlantic meridional overturning circulation to freshwater forcing

Description : Mounting evidence indicates that the Atlantic Meridional Overturning Circulation (AMOC) was strongly reduced during cold climate episodes in the past, possible due to freshwater influx from glacial melting. It is also expected that the freshwater input to high northern latitudes will increase as hum...
Repository : NORA (Norwegian Open Research Archives)
Language(s) : English

Transient response of the Atlantic Meridional Overturning Circulation to enhanced freshwater input to the Nordic Seas–Arctic Ocean in the Bergen Climate Model

Description : The transient response of the climate system to anomalously large freshwater input to the high latitude seas is examined using the newly developed Bergen Climate Model. A 150-yr twin-experiment has been carried out, consisting of a control and a freshwater integration. In the freshwater integration,...
Repository : NORA (Norwegian Open Research Archives)
Language(s) : English

The sensitivity of the present day Atlantic meriodinal overturning circulation to freshwater forcing

Description : Mounting evidence indicates that the Atlantic Meridional Overturning Circulation (AMOC) was strongly reduced during cold climate episodes in the past, possible due to freshwater influx from glacial melting. It is also expected that the freshwater input to high northern latitudes will increase as hum...
Repository : NORA (Norwegian Open Research Archives)
Language(s) : English

Transient response of the Atlantic Meridional Overturning Circulation to enhanced freshwater input to the Nordic Seas–Arctic Ocean in the Bergen Climate Model

Description : The transient response of the climate system to anomalously large freshwater input to the high latitude seas is examined using the newly developed Bergen Climate Model. A 150-yr twin-experiment has been carried out, consisting of a control and a freshwater integration. In the freshwater integration,...
Repository : Bergen Open Research Archive (BORA) - UiB
Language(s) : English

The sensitivity of the present day Atlantic meriodinal overturning circulation to freshwater forcing

Description : Mounting evidence indicates that the Atlantic Meridional Overturning Circulation (AMOC) was strongly reduced during cold climate episodes in the past, possible due to freshwater influx from glacial melting. It is also expected that the freshwater input to high northern latitudes will increase as hum...
Repository : Bergen Open Research Archive (BORA) - UiB
Language(s) : English

Inception of the Northern European Ice Sheet due to contrasting ocean and

Description : About 115,000 years ago the last interglacial reached its terminus and nucleation of new ice sheet growth was initiated. Evidence from the northernmost Nordic Seas indicate that the inception of the last glacial was related to an intensification of the Atlantic Meridional Overturning Circulation ...
Repository : NORA (Norwegian Open Research Archives)
Language(s) : English

Inception of the Northern European Ice Sheet due to contrasting ocean and

Description : About 115,000 years ago the last interglacial reached its terminus and nucleation of new ice sheet growth was initiated. Evidence from the northernmost Nordic Seas indicate that the inception of the last glacial was related to an intensification of the Atlantic Meridional Overturning Circulation ...
Repository : Bergen Open Research Archive (BORA) - UiB
Language(s) : English

Inception of the Northern European Ice Sheet due to contrasting ocean and insolation forcing

Description : About 115,000 years ago the last interglacial reached its terminus and nucleation of new ice sheet growth was initiated. Evidence from the northernmost Nordic Seas indicate that the inception of the last glacial was related to an intensification of the Atlantic Meridional Overturning Circulation ...
Repository : Bergen Open Research Archive (BORA) - UiB
Language(s) : English

Found 20 documents, displaying page 2 of 2