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Typhoons exert significant but differential impacts on net ecosystem carbon exchange of subtropical mangrove forests in China

机译:台风对中国亚热带红树林的净生态系统碳交换产生重大而不同的影响

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Typhoons are very unpredictable natural disturbances to subtropical mangrove forests in Asian countries, but little information is available on how these disturbances affect ecosystem level carbon dioxide (CO_2) exchange of mangrove wetlands. In this study, we examined short-term effect of frequent strong typhoons on defoliation and net ecosystem CO_2 exchange (NEE) of subtropical mangroves, and also synthesized 19 typhoons during a 4-year period between 2009 and 2012 to further investigate the regulation mechanisms of typhoons on ecosystem carbon and water fluxes following typhoon disturbances. Strong wind and intensive rainfall caused defoliation and local cooling effect during the typhoon season. Daily total NEE values decreased by 26-50% following some typhoons (e.g., W28-Nockten, W35-Molave and W35-Lio-Fan), but significantly increased (43-131 %) following typhoon W23-Babj and W38-Megi. The magnitudes and trends of daily NEE responses were highly variable following different typhoons, which were determined by the balance between the variances of gross ecosystem production (GEP) and ecosystem respiration (RE). Furthermore, results from our synthesis indicated that the landfall time of typhoon, wind speed and rainfall were the most important factors controlling the CO_2 fluxes following typhoon events. These findings indicate that different types of typhoon disturbances can exert very different effects on CO_2 fluxes of mangrove ecosystems and that typhoon will likely have larger impacts on carbon cycle processes in subtropical mangrove ecosystems as the intensity and frequency of typhoons are predicted to increase under future global climate change scenarios.
机译:台风是对亚洲国家亚热带红树林的非常不可预测的自然干扰,但是关于这些干扰如何影响红树林湿地的生态系统水平二氧化碳(CO_2)交换的信息很少。在这项研究中,我们研究了频繁的强台风对亚热带红树林的落叶和净生态系统CO_2交换(NEE)的短期影响,并在2009年至2012年的4年期间合成了19个台风,以进一步研究热带气旋的调节机制。台风对生态系统碳和水通量的影响。强风和强降雨造成台风季节的落叶和局部降温作用。某些台风(例如W28-Nockten,W35-Molave和W35-Lio-Fan)发生后,每日总NEE值下降了26-50%,但在W23-Babj和W38-Megi台风之后却显着增加(43-131%)。每天的NEE响应的大小和趋势在不同的台风之后变化很大,这取决于生态系统总产值(GEP)和生态系统呼吸(RE)之间的平衡。此外,我们的综合结果表明,台风登陆时间,风速和降雨是控制台风事件后CO_2通量的最重要因素。这些发现表明,不同类型的台风扰动对红树林生态系统的CO_2通量产生不同的影响,并且随着台风的强度和频率在未来全球范围内增加,台风可能会对亚热带红树林生态系统的碳循环过程产生更大的影响。气候变化情景。

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