Oceanography of the New Zealand subantarctic region

• Main Author: Forcén-Vázquez, Aitana
• Format: Thesis
• Language: unknown
• Published: 2015
• Subjects: Physical Oceanography; Oceanography; Campbell Plateau; Ocean variability; School: School of Geography; Environment and Earth Sciences; 040503 Physical Oceanography; 970104 Expanding Knowledge in the Earth Sciences; Degree Discipline: Geophysics; Degree Level: Doctoral; Degree Name: Doctor of Philosophy; Antarctic; New Zealand; Soi; Antarc*
• Online Access: https://doi.org/10.26686/wgtn.17009291.v1; https://figshare.com/articles/thesis/Oceanography_of_the_New_Zealand_subantarctic_region/17009291

Subantarctic New Zealand is an oceanographycally dynamic region with the Subtropical Front (STF) to the north and the Subantarctic Front (SAF) to the south. This thesis investigates the ocean structure of the Campbell Plateau and the surrounding New Zealand subantarctic, including the spatial, seasonal, interannual and longer term variability over the ocean properties, and their connection to atmospheric variability using a combination of in-situ oceanographic measurements and remote sensing data. The spatial and seasonal oceanographic structure in the New Zealand subantarctic region was investigated by analysing ten high resolution Conductivity Temperature and Depth (CTD) datasets, sampled during oceanographic cruises from May 1998 to February 2013. Position of fronts, water mass structure and changes over the seasons show a complex structure around the Campbell Plateau combining the influence of subtropical and subantarctic waters. The spatial and interannual variability on the Campbell Plateau was described by analysing approximately 70 low resolution CTD profiles collected each year in December between 2002 and 2009. Conservative temperature and absolute salinity profiles reveal high variability in the upper 200m of the water column and a homogeneous water column from 200 to 600m depth. Temperature variability of about 0.7 °C, on occasions between consecutive years, is observed down to 900m depth. The presence of Subantarctic Mode Water (SAMW) on the Campbell Plateau is confirmed and Antarctic Intermediate Water (AAIW) reported for the first time in the deeper regions around the edges of the plateau. Long-term trends and variability over the Campbell Plateau were investigated by analysing satellite derived Sea Level Anomalies (SLA) and Sea Surface Temperature (SST) time series. Links to large scale atmospheric processes are also explored through correlation with the Southern Oscillation Index (SOI) and Southern Annular Mode (SAM). SST shows a strong seasonality and interannual variability which is linked to ...