Article

Science in China Series D: Earth Sciences

, Volume 52, Issue 8, pp 1137-1151

Characteristics of low-frequency oscillation intensity of air-sea turbulent heat fluxes over the northwest Pacific

  • Gen LiAffiliated withSchool of Earth and Space Sciences, University of Science and Technology of China
  • , BaoHua RenAffiliated withSchool of Earth and Space Sciences, University of Science and Technology of China Email author 
  • , JianQiu ZhengAffiliated withSchool of Earth and Space Sciences, University of Science and Technology of China
  • , Jun WangAffiliated withSchool of Earth and Space Sciences, University of Science and Technology of China

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Abstract

Based on the daily turbulent heat fluxes and related meteorological variables datasets (1985–2006) from Objectively Analyzed air-sea Fluxes (OAFlux) Project of Woods Hole Oceanographic Institution (WHOI), characteristics of low-frequency oscillation intensity of air-sea turbulent heat fluxes over the northwest Pacific are analyzed by linear perturbation method and correlation analysis. It can be concluded that: 1) the distribution of low-frequency oscillation intensity of latent heat flux (LHF) over the northwest Pacific is mainly affected by that of low-frequency oscillation intensity of anomalous air-sea humidity gradient (Δq′) as well as mean air-sea humidity gradient (\( \overline {\Delta q} \)), while the distribution of low-frequency oscillation intensity of sensible heat flux (SHF) is mainly affected by that of low-frequency oscillation intensity of anomalous air-sea temperature gradient (ΔT′). 2) The low-frequency oscillation of turbulent heat fluxes over the northwest Pacific is the strongest in winter and the weakest in summer. And the seasonal transition of low-frequency oscillation intensity of LHF is jointly influenced by those of low-frequency oscillation intensity of Δq′, low-frequency oscillation intensity of anomalous wind speed (U′), \( \overline {\Delta q} \) and mean wind speed (Ū), while the seasonal transition of low-frequency oscillation intensity of SHF is mainly influenced by those of low-frequency oscillation intensity of ΔT′ and Ū. 3) Over the tropical west Pacific and sea areas north of 20°N, the low-frequency oscillation of LHF (SHF) is mainly influenced by atmospheric variables q a ′ (T a ′) and U′, indicating an oceanic response to overlying atmospheric forcing. In contrast, over the tropical eastern and central Pacific south of 20°N, q s ′ (T s ′) also greatly influences the low-frequency oscillation of LHF (SHF).

Keywords

northwest Pacific latent heat flux sensible heat flux low-frequency oscillation