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Data on micrometeorological parameters and Energy Fluxes at an intertidal zone of a Tropical Coastal Ocean

机译:热带沿海海洋潮间带微气象参数和能量通量的数据

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摘要

Data on the micrometeorological parameters and Energy Fluxes at an intertidal zone of a Tropical Coastal Ocean was carried out on an installed eddy covariance instruments at a Muka head station in the north-western end of the Pinang Island (5°28’06’’N, 100°12’01’’E), Peninsula Malaysia. The vast source of the supply of energy and heat to the hydrologic and earth׳s energy cycles principally come from the oceans. The exchange of energies via air-sea interactions is crucial to the understanding of climate variability, energy, and water budget. The turbulent energy fluxes are primary mechanisms through which the ocean releases the heat absorbed from the solar radiations to the environment. The eddy covariance (EC) system is the direct technique of measuring the micrometeorological parameters which allow the measurement of these turbulent fluxes in the time scale of half-hourly basis at 20 Hz over a long period. The data being presented is the comparison of the two-year seasonality patterns of monsoons variability on the measured microclimate variables in the southern South China Sea coastal area.
机译:利用位于槟城岛西北端(5°28'06''N的穆卡总站)上安装的涡度协方差仪器对热带沿海海洋潮间带的微气象参数和能量通量进行了数据,100°12'01''E),马来西亚半岛。为水文和地球的能量循环提供能量和热量的主要来源主要来自海洋。通过海气相互作用进行的能量交换对于理解气候变异性,能源和水资源预算至关重要。湍流的能量通量是海洋将太阳辐射吸收的热量释放到环境的主要机制。涡旋协方差(EC)系统是测量微气象参数的直接技术,该技术可以在20?Hz的频率下每半小时的时间范围内长时间测量这些湍流。所提供的数据是南海南部沿海地区季风变率的两年季节性变化与测得的小气候变量的比较。

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