JpGU-AGU Joint Meeting 2017

Presentation information

[EE] Oral

A (Atmospheric and Hydrospheric Sciences) » A-CG Complex & General

[A-CG43] [EE] Air-sea interaction in the extratropics

Sat. May 20, 2017 3:30 PM - 5:00 PM 302 (International Conference Hall 3F)

convener:Kazuaki Nishii(Graduate School of Bioresources, Mie University), Yoshi N Sasaki(Hokkaido University), Shusaku Sugimoto(Graduate School of Science, Tohoku University), Shun Ohishi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Chairperson:Shun Ohishi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Chairperson:Satoru Okajima(Research Center for Advanced Science and Technology)

4:45 PM - 5:00 PM

[ACG43-12] Frontogenesis in the Agulhas Return Current region simulated by a high-resolution CGCM

*Shun Ohishi1, Tomoki Tozuka1, Meghan F. Cronin2 (1.Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo, 2.NOAA Pacific Marine Environmental Laboratory)

Keywords:frontogenesis/frontolysis, Agulhas Return Current, high-resolution coupled general circulation model, horizontal advection, entrainment

Detailed mechanisms for frontogenesis/frontolysis of the sea surface temperature (SST) front in the Agulhas Return Current (ARC) region in the southwestern Indian Ocean are investigated using outputs from a high-resolution coupled general circulation model (CGCM), the Community Earth System Model (CESM; Small et al. 2014), which has good skill in simulating the main features of the SST front and mixed layer depth in the ARC region. The SST front is maintained throughout the year due to approximate balance between frontolysis by surface heat flux and frontogenesis by horizontal advection. Although a southward (northward) cross-isotherm flow on the northern (southern) side of the front is weaker than a strong eastward along-isotherm current in the frontal region, this cross-isotherm confluent flow advects warmer (cooler) temperature toward the SST front north (south) of the front and acts as the dominant frontogenesis mechanism. In addition, stronger (weaker) frontogenesis in austral summer (winter) is attributed to the stronger (weaker) cross-isotherm confluence, which may be linked to seasonal variations of the Agulhas Current, ARC, and Antarctic Circumpolar Current.
On the other hand, the contribution from entrainment is relatively small, because frontolysis by larger (smaller) entrainment velocity on the northern (southern) side opposes frontogenesis by less (more) effective cooling associated with a thicker (thinner) mixed layer and smaller (larger) temperature difference between the mixed layer and entrained water in the northern (southern) region.