Koch M S, Coronado C, Miller M W, Rudnick D T, Stabenau E, Halley R B, Sklar F H
Biological Sciences Department, Florida Atlantic University, 777 Glades Rd, Boca Raton, FL, 33431, USA,
Environ Manage. 2015 Apr;55(4):857-75. doi: 10.1007/s00267-014-0375-y. Epub 2014 Oct 14.
Rising sea levels and temperature will be dominant drivers of coastal Everglades' foundation communities (i.e., mangrove forests, seagrass/macroalgae, and coral reefs) by 2060 based on a climate change scenario of +1.5 °C temperature, +1.5 foot (46 cm) in sea level, ±10 % in precipitation and 490 ppm CO2. Current mangrove forest soil elevation change in South Florida ranges from 0.9 to 2.5 mm year(-1) and would have to increase twofold to fourfold in order to accommodate a 2060 sea level rise rate. No evidence is available to indicate that coastal mangroves from South Florida and the wider Caribbean can keep pace with a rapid rate of sea level rise. Thus, particles and nutrients from destabilized coastlines could be mobilized and impact benthic habitats of southern Florida. Uncertainties in regional geomorphology and coastal current changes under higher sea levels make this prediction tentative without further research. The 2060 higher temperature scenario would compromise Florida's coral reefs that are already degraded. We suggest that a new paradigm is needed for resource management under climate change that manages coastlines for resilience to marine transgression and promotes active ecosystem management. In the case of the Everglades, greater freshwater flows could maximize mangrove peat accumulation, stabilize coastlines, and limit saltwater intrusion, while specific coral species may require propagation. Further, we suggest that regional climate drivers and oceanographic processes be incorporated into Everglades and South Florida management plans, as they are likely to impact coastal ecosystems, interior freshwater wetlands and urban coastlines over the next few decades.
根据气温上升1.5摄氏度、海平面上升1.5英尺(46厘米)、降水量变化±10%以及二氧化碳浓度达到490 ppm的气候变化情景,到2060年,海平面上升和气温升高将成为沿海大沼泽地基础群落(即红树林、海草/大型藻类和珊瑚礁)的主要驱动因素。南佛罗里达州目前红树林土壤高程变化范围为每年0.9至2.5毫米,为适应2060年的海平面上升速度,这一变化速度必须提高两倍至四倍。目前尚无证据表明南佛罗里达州和更广泛的加勒比地区的沿海红树林能够跟上快速的海平面上升速度。因此,不稳定海岸线的颗粒和养分可能会被调动起来,影响佛罗里达州南部的底栖生境。在海平面上升的情况下,区域地貌和沿海洋流变化的不确定性使得这一预测具有不确定性,需要进一步研究。2060年的高温情景将危及佛罗里达州已经退化的珊瑚礁。我们建议,在气候变化背景下的资源管理需要一种新的范式,即管理海岸线以增强抵御海侵的能力,并促进积极的生态系统管理。就大沼泽地而言,增加淡水流量可以使红树林泥炭积累最大化、稳定海岸线并限制海水入侵;而对于特定的珊瑚物种,可能需要进行繁殖。此外,我们建议将区域气候驱动因素和海洋学过程纳入大沼泽地和南佛罗里达州的管理计划,因为它们可能在未来几十年影响沿海生态系统、内陆淡水湿地和城市海岸线。