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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 mangroveforests in Asian countries, but little information is available on how thesedisturbances affect ecosystem level carbon dioxide (CO2) exchange ofmangrove wetlands. In this study, we examined short-term effect of frequentstrong typhoons on defoliation and net ecosystem CO2 exchange (NEE) ofsubtropical mangroves, and also synthesized 19 typhoons during a 4-yearperiod between 2009 and 2012 to further investigate the regulationmechanisms of typhoons on ecosystem carbon and water fluxes followingtyphoon disturbances. Strong wind and intensive rainfall caused defoliationand local cooling effect during the typhoon season. Daily total NEE valuesdecreased 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 dailyNEE responses were highly variable following different typhoons, which weredetermined by the balance between the variances of gross ecosystemproduction (GEP) and ecosystem respiration (RE). Furthermore, results fromour synthesis indicated that the landfall time of typhoon, wind speed andrainfall were the most important factors controlling the CO2 fluxesfollowing typhoon events. These findings indicate that different types oftyphoon disturbances can exert very different effects on CO2 fluxes ofmangrove ecosystems and that typhoon will likely have larger impacts oncarbon cycle processes in subtropical mangrove ecosystems as the intensityand frequency of typhoons are predicted to increase under future globalclimate change scenarios.
机译:台风是亚洲国家对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,我们研究了强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,以进一步研究台风对台风干扰后生态系统碳和水通量的调节机制。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,则显着增加(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控制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,而且台风强度和频率预计将对亚热带红树林生态系统的碳循环过程产生更大的影响。在未来的全球气候变化情景下增长。

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