Auflistung nach Mitwirkenden "Brandt, Peter"
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Fluctuations of the Atlantic North Equatorial Undercurrent and Associated Changes in Oxygen Transports
Burmeister, Kristin; Luebbecke, Joke F.; Brandt, Peter; Claus, Martin; Hahn, Johannes (Geophysical Research Letters, 2020)Abstract Although the core velocity of the Atlantic North Equatorial Undercurrent (NEUC) is low (0.1−0.3 m s−1), it has been suggested to act as an important oxygen supply route towards the oxygen minimum zone in the ... -
Impact of Intraseasonal Waves on Angolan Warm and Cold Events
The intraseasonal variability of the tropical eastern boundary upwelling region in the Atlantic Ocean is investigated using multiyear mooring and satellite data. Pronounced oscillations of alongshore velocity and sea level ... -
Origin of Weakened Interannual Sea Surface Temperature Variability in the Southeastern Tropical Atlantic Ocean
Prigent, Arthur; Imbol Koungue, Rodrigue Anicet; Lübbecke, Joke F.; Brandt, Peter; Latif, Mojib (Geophysical Research Letters, 2020)Observations and reanalysis products are used to investigate the substantial weakening in the southeastern tropical Atlantic sea surface temperature (SST) variability since 2000. Relative to 1982–1999, the March-April-May ... -
Transports and Pathways of the Tropical AMOC Return Flow From Argo Data and Shipboard Velocity Measurements
Tuchen, Franz Philip; Brandt, Peter; Lübbecke, Joke F.; Hummels, Rebecca (Journal of Geophysical Research: Oceans, 2022-02-05)The upper‐ocean circulation of the tropical Atlantic is a complex superposition of thermohaline and wind‐driven flow components. The resulting zonally and vertically integrated upper‐ocean meridional flow is referred to ... -
Tropical Instability Waves and Wind‐Forced Cross‐Equatorial Flow in the Central Atlantic Ocean
Heukamp, Finn Ole; Brandt, Peter; Dengler, Marcus; Tuchen, Franz Philip; McPhaden, Michael J.; Moum, James N. (Geophysical Research Letters, 2022-09-29)Based on velocity data from a long‐term moored observatory located at 0°N, 23°W we present evidence of a vertical asymmetry during the intraseasonal maxima of northward and southward upper‐ocean flow in the equatorial ...