Sensible, latent heat and store energy fluxes in the suburban São Paulo Megacity: seasonal and interannual variations and empirical modeling

Flávia Dias Rabelo Torres, Amauri Pereira de Oliveira, Lucas Cardoso da Silveira
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Abstract

Half-hourly values of turbulent sensible (H) and latent (LE) heat fluxes, net radiation (𝑄∗) at the surface, and heat store in the canopy (𝛥𝑄𝑆) are used to characterize seasonal and interannual changes during three not-consecutive years (2009–12) in a suburban area (LCZ 6) of the megacity of São Paulo. Turbulent fluxes are estimated applying eddy covariance method to turbulence measurements performed with sampling rate of 10 Hz, between 25 and 26 m above the surface, and enforcing quality control procedures. The diurnal evolution of monthly average hourly values of 𝐻, 𝐿𝐸, 𝑄∗ and 𝛥𝑄𝑆 observed in 2012 indicate a seasonal variation with a daytime maximum with 𝐻 varying from a maximum of 180 ± 12 W m-2 in October to a minimum of 80.1 ± 9 W m2 in June, 𝐿𝐸 varying from a maximum of 152.0 ± 7.6 W m-2 in February to a minimum of 66.4 ± 7.6 W m-2 in September, -𝑄∗ varying from a maximum of 554 ± 14 W m-2 in February to a minimum of 369±13 W m-2 in July, and -𝛥𝑄𝑆 varying from a maximum of 249± 47 W m-2 in April to a minimum of 181 ± 58 W m-2 in July. Monthly average daily values of H, LE and 𝑄∗ corroborate seasonal pattern displayed by monthly average hourly values, with maximum of 5 ± 0.5 MJ m-2 day-1 for H and 5.3 ± 0.6 MJ m-2 day-1 for LE in November (summer), and minimum of 1.3 ± 0.2 MJ m-2 day-1 for H in June and 1.9 ± 0.2 MJ m-2 day-1 for LE in August. −𝑄∗ shows a maximum of 11.6 ± 1.1 MJ m2 day-1 in March and a minimum of 4.5±0.9 MJ m-2 day-1 in June. Similar patterns was observed during 2009 and 2010. An empirical model based on Modified Priestly-Taylor Method coupled to Objective Hysteresis Method was validated with observations carried out during May and June (2009–2010, 2012) and applied successfully to estimate monthly average hourly values of 𝐻, LE and 𝛥𝑄𝑆 during February–April and August–Novemb 2012.
圣保罗特大城市郊区的感热、潜热和蓄能通量:季节和年际变化和经验模型
利用半小时湍流感热通量(H)和潜热通量(LE)、地表净辐射(𝑄∗)和冠层热储量(𝛥𝑄𝑆)的数值,描述了大城市圣保罗郊区(lcz6) 3个非连续年(2009-12)的季节和年际变化。湍流通量估计应用涡动相关法进行湍流测量,采样率为10赫兹,在25和26米之间的表面,并执行质量控制程序。月平均每小时的昼夜演化的价值观𝐻,𝐿𝐸,𝑄∗和𝛥𝑄𝑆2012年的观察显示出季节性变化与白天最大𝐻不同从最高的180±12 W m - 2 10月最低为80.1±6月9 W m2,𝐿𝐸不同从最高152.0±7.6 W m - 2 2月最低为66.4±7.6 W m - 2 9月——𝑄∗不同从最高的554±14 W m - 2 369年2月的最低±7月13 W m - 2,-𝛥𝑄𝑆4月最大值为249±47 wm -2, 7月最小值为181±58 wm -2。H、LE和𝑄*的月平均日值与月平均小时值所显示的季节特征一致,11月(夏季)H的最大值为5±0.5 MJ m-2 day-1, LE的最大值为5.3±0.6 MJ m-2 day-1, 6月H的最小值为1.3±0.2 MJ m-2 day-1, 8月LE的最小值为1.9±0.2 MJ m-2 day-1。−𝑄* 3月最大值为11.6±1.1 MJ m2 day-1, 6月最小值为4.5±0.9 MJ m-2 day-1。2009年和2010年也出现了类似的情况。利用2012年5月和6月(2009-2010年、2012年)的观测数据,对基于修正Priestly-Taylor法和客观滞后法的实证模型进行了验证,并成功估算了2012年2 - 4月和8 - 11月𝐻、LE和𝛥𝑄𝑆的月平均时值。
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