U.S. Geological Survey, Northern Rocky Mountain Science Center, 2327 University Way, Suite 2, Bozeman, MT, 59715, USA.
Glob Chang Biol. 2013 Oct;19(10):3069-81. doi: 10.1111/gcb.12262. Epub 2013 Jun 21.
We combine large observed data sets and dynamically downscaled climate data to explore historic and future (2050-2069) stream temperature changes over the topographically diverse Greater Yellowstone Ecosystem (elevation range = 824-4017 m). We link future stream temperatures with fish growth models to investigate how changing thermal regimes could influence the future distribution and persistence of native Yellowstone cutthroat trout (YCT) and competing invasive species. We find that stream temperatures during the recent decade (2000-2009) surpass the anomalously warm period of the 1930s. Climate simulations indicate air temperatures will warm by 1 °C to >3 °C over the Greater Yellowstone by mid-21st century, resulting in concomitant increases in 2050-2069 peak stream temperatures and protracted periods of warming from May to September (MJJAS). Projected changes in thermal regimes during the MJJAS growing season modify the trajectories of daily growth rates at all elevations with pronounced growth during early and late summer. For high-elevation populations, we find considerable increases in fish body mass attributable both to warming of cold-water temperatures and to extended growing seasons. During peak July to August warming, mid-21st century temperatures will cause periods of increased thermal stress, rendering some low-elevation streams less suitable for YCT. The majority (80%) of sites currently inhabited by YCT, however, display minimal loss (<10%) or positive changes in total body mass by midcentury; we attribute this response to the fact that many low-elevation populations of YCT have already been extirpated by historical changes in land use and invasions of non-native species. Our results further suggest that benefits to YCT populations due to warmer stream temperatures at currently cold sites could be offset by the interspecific effects of corresponding growth of sympatric, non-native species, underscoring the importance of developing climate adaptation strategies that reduce limiting factors such as non-native species and habitat degradation.
我们结合了大量观测数据集和动态下推的气候数据,探索了地形多样的大黄石生态系统(海拔范围=824-4017 米)过去和未来(2050-2069 年)的溪流温度变化。我们将未来的溪流温度与鱼类生长模型联系起来,研究热环境变化如何影响黄石溪红点鲑(YCT)和竞争入侵物种的未来分布和持续存在。我们发现,近十年(2000-2009 年)的溪流温度超过了 20 世纪 30 年代异常温暖的时期。气候模拟表明,到 21 世纪中叶,大黄石地区的空气温度将升高 1°C 到>3°C,导致 2050-2069 年高峰溪流温度和 5 月至 9 月(MJJAS)持续变暖的相应增加。在 MJJAS 生长季节,热环境变化的预测变化改变了所有海拔高度的日生长率轨迹,夏季早期和晚期生长明显。对于高海拔地区的种群,我们发现由于冷水温度变暖以及生长季节延长,鱼类体质量的增加相当大。在 7 月至 8 月高峰变暖期间,21 世纪中叶的温度将导致热应激增加的时期,使一些低海拔溪流对 YCT 的适应性降低。然而,目前 YCT 栖息的大多数(80%)地点显示出最小的损失(<10%)或总体质量的积极变化到本世纪中叶;我们将这种反应归因于许多低海拔 YCT 种群已经由于土地利用历史变化和非本地物种的入侵而灭绝的事实。我们的研究结果进一步表明,由于目前寒冷地区溪流温度升高对 YCT 种群的益处可能会被共生非本地物种相应生长的种间效应所抵消,突出了制定减少非本地物种和栖息地退化等限制因素的气候适应策略的重要性。