关键词:
Ocean currents
Wind
Basins
Regions
Maps
Decomposition
Ocean circulation
Energy
Algorithms
Time series
Climate
Computer science
Geomorphology
Geology
摘要:
Over recent decades, changes in the climate system have fundamentally modified properties of the ocean. These adjustments include alterations of the sea level, the sea surface temperature, and the ocean circulation from regional to global scales. The ocean surface responds to changes in the climate system through the exchange of heat, carbon, and momentum. Numerous studies have examined the response of sea level and ocean heat content to climate change; however, it remains unknown how the ocean surface currents have adjusted to the climate system over the past decades. Ocean currents have a wide range of spatial and temporal scales, from submesoscales (100m to 10 km), to mesoscale (10 to 100 km), to large-scale overturning. Dynamically, mesoscale flows are crucial in the transport and mixing of tracers such as heat, salt, and nutrients, but they also constitute one of the major reservoirs of the time-varying kinetic energy, namely eddy kinetic energy (EKE). Mesoscale flows consist of three distinct processes: coherent eddies, jets, and waves. The temporal evolution of the ocean currents and the mesoscale field is yet to be quantified. In this thesis, we use satellite observations and a coherent eddy tracking algorithm (Track: Eddy) to investigate the temporal evolution of the surface mesoscale, coherent eddies, and jets over the last 27 years. We find a multi-decadal readjustment of the eddy and mesoscale field to changes in the climate system from two independent satellite products. Eddy kinetic energy and sea surface temperature gradients show a significant strengthening of the eddy field at rates of 1.2%-1.8% per decade. Furthermore, regions dominated by mesoscale processes such as the Antarctic Circumpolar Current (ACC) and ocean boundary currents have undergone a greater change over the observational record at rates of 5% and 2.5% per decade, respectively. This global and regional readjustment of the surface currents has crucial implications in the exchange of