Annual evolution of the ice–ocean interaction beneath landfast ice in Prydz Bay, East Antarctica
High-frequency observations of the ice–ocean interaction and high-precision estimation of the ice–ocean heat exchange are critical to understanding the thermodynamics of the landfast ice mass balance in Antarctica. To investigate the oceanic contribution to the evolution of the landfast ice, an inte...
| Published in: | The Cryosphere |
|---|---|
| Main Authors: | , , , , , , |
| Format: | Text |
| Language: | English |
| Published: |
2023
|
| Subjects: | |
| Online Access: | https://doi.org/10.5194/tc-17-2231-2023 https://tc.copernicus.org/articles/17/2231/2023/ |
| Summary: | High-frequency observations of the ice–ocean interaction and high-precision estimation of the ice–ocean heat exchange are critical to understanding the thermodynamics of the landfast ice mass balance in Antarctica. To investigate the oceanic contribution to the evolution of the landfast ice, an integrated ocean observation system, including an acoustic Doppler velocimeter (ADV), conductivity–temperature–depth (CTD) sensors, and a sea ice mass balance array (SIMBA), was deployed on the landfast ice near the Chinese Zhongshan Station in Prydz Bay, East Antarctica, from April to November 2021. The CTD sensors recorded the ocean temperature and salinity. The ocean temperature experienced a rapid increase in late April, from − 1.62 to the maximum of − 1.30 ∘ C, and then it gradually decreased to − 1.75 ∘ C in May and remained at this temperature until November. The seawater salinity and density exhibited similar increasing trends during April and May, with mean rates of 0.04 psu d −1 and 0.03 kg m −3 d −1 , respectively, which was related to the strong salt rejection caused by freezing of the landfast ice. The ocean current observed by the ADV had mean horizontal and vertical velocities of 9.5 ± 3.9 and 0.2 ± 0.8 cm s −1 , respectively. The domain current direction was ESE (120 ∘ )–WSW (240 ∘ ), and the domain velocity (79 %) was 5–15 cm s −1 . The oceanic heat flux ( F w ) estimated using the residual method reached a peak of 41.3 ± 9.8 W m −2 in April, and then it gradually decreased to a stable level of 7.8 ± 2.9 W m −2 from June to October. The F w values calculated using three different bulk parameterizations exhibited similar trends with different magnitudes due to the uncertainties of the empirical friction velocity. The spectral analysis results suggest that all of the observed ocean variables exhibited a typical half-day period, indicating the strong diurnal influence of the local tidal oscillations. The large-scale sea ice distribution and ocean circulation contributed to the seasonal variations in the ... |
|---|