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Interannual changes in the overflow from the Nordic Seas into the Atlantic Ocean through Denmark Strait

• Albert Macrander, Uwe Send, Helgi Valdimarsson, Sigurjon Jonsson, Rolf H. Käse
• 2005

[1] The global thermohaline circulation is an important part of Earth’s climate system. Cold, dense water formed in the Nordic Seas enters the Atlantic Ocean as overflows across the sills of the… (More)

Observation of decadal change in the Atlantic meridional overturning circulation using 10 years of continuous transport data

• Uwe Send, Matthias Lankhorst, Torsten Kanzow
• 2011

[1] The meridional overturning circulation (MOC) represents the main mechanism for the oceanic northward heat transport in the Atlantic, and fluctuations of this circulation are believed to have… (More)

Amplification of hypoxic and acidic events by La Niña conditions on the continental shelf off California

• SungHyun Nam, Hey-Jin Kim, Uwe Send
• 2011

[1] Low-oxygen and low-pH events are an increasing concern and threat in the Eastern Pacific coastal waters, and can be lethal for benthic and demersal organisms on the continental shelf. The normal… (More)

The ocean takes a deep breath.

• A Körtzinger, Jens Schimanski, Uwe Send, Douglas Wallace
• Science
• 2004

Deep convection is the major mechanism for replenishing oxygen in the deep interior of the world ocean, and its variability affects the use of atmospheric oxygen to monitor the global carbon cycle.… (More)

Seasonal variation of ocean bottom pressure derived from Gravity Recovery and Climate Experiment ( GRACE ) : Local validation and global patterns

• Torsten Kanzow, Frank Flechtner, Alan D. Chave, Roland Schmidt, Peter Schwintzer, Uwe Send
• 2005

[1] The Gravity Recovery and Climate Experiment (GRACE) processing centers at the GeoForschungsZentrum Potsdam (GFZ) and the University of Texas Center for Space Research (UTCSR) provide time series… (More)

Relaxation from upwelling: The effect on dissolved oxygen on the continental shelf

• Uwe Send, SungHyun Nam
• 2012

[1] Continental shelves in upwelling regimes are subject to sequences of upwelling and relaxation events, each on timescales of order 1 week typically. These episodes have pronounced impacts on the… (More)

Acoustic observations of heat content across the Mediterranean Sea

• Uwe Send, Gerd Krahmann, +7 authors Claude Millot
• 1997

The ability to monitor the heat content of oceans over long distances is becoming increasingly important for understanding the role of oceans in climate change, for determining the variability of the… (More)

Direct evidence of deep water intrusions onto the continental shelf via surging internal tides

• SungHyun Nam, Uwe Send
• 2011

[1] Near‐bottom diurnal thermocline shoaling and diurnal baroclinic currents were observed from time series data of water temperature, salinity, pressure, and velocity collected from August 2006 to… (More)

Interannual variability of newly formed Labrador Sea Water from 1994 to 2005

• Tom Avsic, J Karstensen, Uwe Send, Juergen Fischer
• 2006

[1] Mooring records collected in the central Labrador Sea are evaluated regarding the variability of the hydrographic properties of newly formed Labrador Sea Water (LSW) between 1994 and 2005. This… (More)

A GLOBAL BOUNDARY CURRENT CIRCULATION OBSERVING NETWORK

• Uwe Send, Robert Davis, +10 authors Laura Beal
• 2011

Western and eastern boundary currents are key regions for understanding and monitoring the ocean's influence on and response to climate change processes. Yet the present global ocean observing is… (More)

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