## A13J-3301: Impacts of Regional Mixing on the Temperature Structure of the Equatorial Pacific Ocean. Part 2: Depth-Dependent Vertical Diffusion

Monday, 15 December 2014
Ryo Furue1,2, Yanli Jia1 and Julian P McCreary Jr1, (1)IPRC Univ of Hawaii, Honolulu, HI, United States, (2)JAMSTEC Japan Agency for Marine-Earth Science and Technology, Kanagawa, Japan
##### Abstract:
In this study, we use an ocean model to explore how vertical mixing influences temperature in the eastern equatorial Pacific Ocean (EEPO). Our approach is to change the background diffusion coefficient from a constant value κb$\kappa_{b}$ to κb+δκ(z)$\kappa_{b}+\delta\kappa(z)$ in various subregions of the tropical Pacific, and then to determine the resulting temperature changes in the near-equilibrium response. In a companion paper (Furue et al., 2014, submitted), we consider the impacts of depth-independent κb$\kappa_b$ anomalies. Here, we examine the impacts of depth-dependent anomalies that are confined above, or centered on, the mid-depth of the pycnocline.

During the first year of adjustment, solutions develop a local temperature response that results largely from the one-dimensional balance, δTt=(δκTz)z=δκzTz+δκTzz$\delta T_{t} = (\delta\kappa T_{z})_{z} = \delta\kappa_{z}T_{z}+\delta\kappa T_{zz}$, with a similar equation for salinity. At this stage, δκ$\delta\kappa$ generates temperature and salinity anomalies that are either associated with a density change (dynamical anomalies) or without one (spiciness anomalies). Subsequently, dynamical and spiciness anomalies spread to remote regions by wave radiation and advection, respectively.

For positive δκ$\delta\kappa$ anomalies confined above the mid-pycnocline, δκzTz$\delta\kappa_{z}T_{z}$ (δκTzz$\delta\kappa T_{zz}$) tends to produce positive (negative) temperature anomalies, which spread to the equator dynamically (by wave radiation) and are still apparent in near-equilibrium solutions. For δκ$\delta\kappa$ anomalies confined within the pycnocline (with monopole, dipole, and tripole profiles), the response is dominated by δκzTz$\delta\kappa_{z}T_{z}$, owing to δκ$\delta\kappa$ having a smaller vertical scale than T$T$ and to δκ$\delta\kappa$ not overlapping well with Tzz$T_{zz}$; the resulting temperature anomalies tend to shift the pycnocline vertically (dipole profile) or to alter its thickness (monopole and tripole profiles).

Positive anomalies from all subregions contribute to an increase of near-surface (upper 50 m) temperature in the EEPO, the amplitude and location of the warming depending on the depth range of the warming band generated within the locally forced subregion.