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Impact of Hurricane Sandy on CH4 Released from Vegetated and Unvegetated Wetland Microsites

机译:桑迪飓风对无植被和无植被湿地微场所释放的CH4的影响

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Hurricane Sandy was one of the largest tropical storms to pass over the Atlantic basin, causing destruction along its path as it made landfall in Jamaica, Cuba, the Bahamas, and the United States [Tropical Cyclone Report: Hurricane Sandy; National Weather Service, National Oceanic and Atmospheric Administration, 2012 (http://www.nhc.noaa.gov/data/tcr/ AL182012_Sandy)]. Hurricane Sandy passed over the Meadow- lands in the midst of our multiyear study on marsh CH4 dynamics, providing a unique opportunity to evaluate the effects of hurricanes on CH4 cycling within an estuarine marsh. We modeled dissolved CH4 distributions in wetland sediments from 2011 (Reid, M. C.; Tripathee, R.; Shafer, K. V. R.; Jaffe,P.R. Tidal Marsh Methane dynamics: Difference in seasonal lags in emissions driven by storage in vegetated versus unvegetated sediments. J. Geophys. Res.: Biogeosci. 2013, 118, 1802-1813) to 2013 and estimated that Hurricane Sandy did not degas vegetated soils but degassed between 45 and 75% of the dissolved CH4 in unvegetated sediments. Hurricanes may regularly affect coastal wetland CH4 emissions globally, but because these wetland sediments do not store substantial dissolved CH4 late in the year, the degassing of these sediments by Hurricane Sandy did not play an important role in the annual carbon emissions from this marsh.
机译:桑迪飓风是穿越大西洋盆地的最大热带风暴之一,在其登陆牙买加,古巴,巴哈马和美国时造成沿途的破坏[热带气旋报告:飓风桑迪;国家气象局,国家海洋与大气管理局,2012年(http://www.nhc.noaa.gov/data/tcr/ AL182012_Sandy)]。在我们关于沼泽CH4动力学的多年研究中,桑迪飓风越过了草地,为评估飓风对河口沼泽中CH4循环的影响提供了独特的机会。我们对2011年以来湿地沉积物中的溶解CH4分布进行了建模(Reid,MC; Tripathee,R .; Shafer,KVR; Jaffe,PR潮汐沼气)甲烷动力学:植被和非植被沉积物存储驱动的排放季节性滞后差异。 Res .: Biogeosci。2013,118,1802-1813)至2013年,并估计飓风桑迪并未对植被土壤脱气,但对未植被沉积物中溶解的CH4的45%至75%进行了脱气。飓风可能会定期影响全球沿海湿地CH4的排放,但是由于这些湿地沉积物在年底未储存大量溶解的CH4,因此飓风桑迪对这些沉积物进行脱气在该沼泽每年的碳排放中没有发挥重要作用。

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