Year-round observations of sea-ice drift and near-inertial internal waves in the Northwind Abyssal Plain, Arctic Ocean
| Autor: | Takashi Kikuchi, Motoyo Itoh, Naomi Harada, Yasushi Fukamachi, Yusuke Kawaguchi, Jonaotaro Onodera, Erika Moriya |
|---|---|
| Rok vydání: | 2019 |
| Předmět: |
0106 biological sciences
010504 meteorology & atmospheric sciences Aquatic Science 01 natural sciences Sonar Physics::Geophysics Acoustic Doppler current profiler Internal gravity waves Sea ice Inertial oscillation Physics::Atmospheric and Oceanic Physics Ecology Evolution Behavior and Systematics 0105 earth and related environmental sciences geography geography.geographical_feature_category Ecology 010604 marine biology & hydrobiology Abyssal plain Internal wave Mooring Geodesy Ice profiling sonar Amplitude Arctic General Earth and Planetary Sciences Ice drift Astrophysics::Earth and Planetary Astrophysics Arctic ocean Geology |
| Zdroj: | Polar Science. 21:212-223 |
| ISSN: | 1873-9652 |
| Popis: | In this study, intra-annual variation of near-inertial internal wave (NIW) in the Arctic Ocean is examined using year-round mooring in the Northwind Abyssal Plain. Our emphasis is on dynamical responses of NIW to local sea-ice variables such as concentration, draft, and drift. We obtained those using a coupling system of ice profiling sonar (IPS) and an acoustic Doppler current profiler (ADCP) deployed at the top of the mooring. According to the wavelet spectrum, the inertial oscillation of ice drift becomes considerably strong during periods of ice formation and decay. Results show that the NIW amplitude in the upper part of the water column responds more sensitively to the sea-ice inertial oscillation than to the mean component of ice drift heading to the northwest. We also conducted an experiment with a mixed-layer slab model using the IPS-ADCP measured ice speed to examine the NIW generation responding to the ice-to-ocean stress. Experiment results suggest that the mixed-layer inertial oscillation is amplified in the early time of ice formation, through the ice-water resonance process. It is then concluded that the mixed-layer inertial current driven by ice drift is the primary driver of the enhanced NIW generation. |
| Databáze: | OpenAIRE |
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