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Comparison of the mass and energy exchange of a pasture and a mature transitional tropical forest of the southern Amazon Basin during a seasonal transition

机译:季节性过渡期间南部亚马逊河流域的牧场和成熟的过渡热带森林的质量和能量交换比较

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This research utilized tower-based eddy covariance to quantify the trends in net ecosystem mass (CO2 and H2O vapor) and energy exchange of important land-cover types of NW Mato Grosso during the March-December 2002 seasonal transition. Measurements were made in a mature transitional (ecotonal) tropical forest near Sinop, Mato Grosso, and a cattle pasture near Cotriguacu, Mato Grosso, located 500 km WNW of Sinop. Pasture net ecosystem CO2 exchange (NEE) was considerably more variable than the forest NEE over the seasonal transition, and the pasture had significantly higher rates of maximum gross primary production in every season except the dry-wet season transition (September-October). The pasture also had significantly higher rates of whole-ecosystem dark respiration than the forest during the wetter times of the year. Average (+/-95% CI) rates of total daily NEE during the March-December 2002 measurement period were 26+/-15 mmol m(-2) day(-1) for the forest (positive values indicate net CO2 loss by the ecosystem) and -38+/-26 mmol m(-2) day(-1) for the pasture. While both ecosystems partitioned more net radiation (R-n) into latent heat flux (L-e), the forest had significantly higher rates of L-e and lower rates of sensible heat flux (H) than the pasture; a trend that became more extreme during the onset of the dry season. Large differences in pasture and forest mass and energy exchange occurred even though seasonal variations in micrometeorology (air temperature, humidity, and radiation) were relatively similar for both ecosystems. While the short measurement period and lack of spatial replication limit the ability to generalize these results to pasture and forest regions of the Amazon Basin, these results suggest important differences in the magnitude and seasonal variation of NEE and energy partitioning for pasture and transitional tropical forest.
机译:这项研究利用基于塔的涡动协方差来量化2002年3月至12月季节性过渡期间净生态系统质量(CO2和H2O蒸气)和重要的土地覆盖类型的能量交换的趋势。测量是在马诺格罗索州锡诺普附近的一个成熟的过渡(生态)热带森林中,以及位于锡诺普西北方500公里处的马托格罗索州科特里瓜库附近的一个牛牧场中进行的。在整个季节过渡期中,牧场净生态系统CO2交换(NEE)的变化程度要比森林NEE大得多,并且除干湿季节过渡期(9月至10月)外,每个季节的牧草的最高初级总产值均显着较高。在一年的湿润时间里,牧场的全生态系统暗呼吸速率也比森林高得多。 2002年3月至12月测量期间,森林的每日平均NEE的平均比率(+/- 95%CI)为26 +/- 15 mmol m(-2)天(-1)(正值表明,生态系统)和-38 +/- 26 mmol m(-2)天(-1)(牧场)。虽然这两个生态系统都将更多的净辐射(R-n)划分为潜热通量(L-e),但与牧场相比,森林的L-e率显着较高,而感热通量(H)则较低。这种趋势在旱季开始时变得更加极端。尽管两种生态系统的微气象学的季节性变化(气温,湿度和辐射)相对相似,但牧场和森林的质量与能量交换仍存在很大差异。尽管测量周期短和缺乏空间复制限制了将这些结果推广到亚马逊河流域的牧场和森林区域的能力,但这些结果表明,NEE的大小和季节变化以及牧场和过渡热带森林的能量分配存在重要差异。

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