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Temporal and spatial patterns of remotely sensed litterfall in tropical and subtropical forests of Taiwan

机译:台湾热带和亚热带森林中遥感凋落物的时空格局

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Litterfall is important for returning nutrients and carbon to the forest floor, andmicrobes decompose the litterfall to release CO_2 into the atmosphere. Litterfall is a pivotal component in the forest biogeochemical cycle, which is sensitive to climate variability and plant physiology. In this study, we combined field litterfall estimates and time series (2001–2011) climate (theModerate Resolution Imaging Spectroradiometer (MODIS) land surface temperature (LST) and Tropical Rainfall Measuring Mission (TRMM) precipitations) and green vegetation (MODIS photosynthetically active vegetation cover (PV)) variables to estimate regional annual litterfall in tropical/subtropical forests in Taiwan. We found that time series MODIS LST- and PV-derived metrics, the annual accumulated MODIS LST, and coefficient of variation of PV, respectively, but not the TRMM precipitation variables were salient factors for the estimation (r~2=0.548 and p<0.001). The mean (±standard deviation) annual litterfall was 5.1 ± 1.2Mgha~(-1) yr~(-1) during the observation period. The temporal dynamics of the litterfall revealed that typhoons and consecutive drought events might affect the litterfall temporal variation. Overall, the annual litterfall decreased along the elevation gradient, which may reflect a change in the vegetation type. The northeast and northwest facing slopes yielded the highest amount of annual litterfall (≥5.9Mg ha~(-1) yr~(-1)), which was in contrast with the southern aspect (5.1Mgha~(-1) yr~(-1)). This variation may be associatedwith the dryness of the microclimate influenced by solar radiation. This study demonstrates the feasibility of utilizing time seriesMODIS LST and PV data to predict large-scale field litterfall, which may facilitate large-scale monitoring of biogeochemical cycles in forest ecosystems.
机译:凋落物对于将养分和碳返回到森林地面非常重要,微生物分解凋落物以将CO_2释放到大气中。凋落物是森林生物地球化学循环中的关键组成部分,对气候变化和植物生理非常敏感。在这项研究中,我们结合了田间凋落物估计和时间序列(2001-2011年)的气候(中等分辨率成像光谱仪(MODIS)地表温度(LST)和热带降雨测量任务(TRMM)的降水)和绿色植被(MODIS光合作用的植被)覆盖(PV)变量,以估算台湾热带/亚热带森林的区域凋落物。我们发现时间序列MODIS LST和PV派生的度量标准,年累积MODIS LST和PV的变异系数,但TRMM降水变量不是估算的显着因素(r〜2 = 0.548和p < 0.001)。观测期内年平均凋落物数(±标准偏差)为5.1±1.2Mgha〜(-1)yr〜(-1)。凋落物的时间动态表明,台风和连续的干旱事件可能影响凋落物的时间变化。总体而言,年度凋落物沿海拔梯度下降,这可能反映了植被类型的变化。东北和西北面向的斜坡产生的年度凋落物数量最高(≥5.9Mgha〜(-1)yr〜(-1)),与南部地区相反(5.1Mgha〜(-1)yr〜(-1)。 -1))。这种变化可能与受太阳辐射影响的小气候的干燥有关。这项研究证明了利用时间序列MODIS LST和PV数据预测大规模田间凋落物的可行性,这可能有助于对森林生态系统中生物地球化学循环进行大规模监测。

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