Kimball Kenneth D, Davis Michael L, Weihrauch Douglas M, Murray Georgia L D, Rancourt Kenneth
Research Department, Appalachian Mountain Club, 361 Route 16, Gorham, New Hampshire 03581 USA.
Research Department, Appalachian Mountain Club, 361 Route 16, Gorham, New Hampshire 03581 USA Ecology Center, Utah State University, 5205 Old Main Hill-NR 314, Logan, Utah 84322 USA.
Am J Bot. 2014 Sep;101(9):1437-46. doi: 10.3732/ajb.1400214. Epub 2014 Sep 14.
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Most alpine plants in the Northeast United States are perennial and flower early in the growing season, extending their limited growing season. Concurrently, they risk the loss of reproductive efforts to late frosts. Quantifying long-term trends in northeastern alpine flower phenology and late-spring/early-summer frost risk is limited by a dearth of phenology and climate data, except for Mount Washington, New Hampshire (1916 m a.s.l.).•
Logistic phenology models for three northeastern US alpine species (Diapensia lapponica, Carex bigelowii and Vaccinium vitis-idaea) were developed from 4 yr (2008-2011) of phenology and air temperature measurements from 12 plots proximate to Mount Washington's long-term summit meteorological station. Plot-level air temperature, the logistic phenology models, and Mount Washington's climate data were used to hindcast model yearly (1935-2011) floral phenology and frost damage risk for the focal species.•
Day of year and air growing degree-days with threshold temperatures of -4°C (D. lapponica and C. bigelowii) and -2°C (V. vitis-idaea) best predicted flowering. Modeled historic flowering dates trended significantly earlier but the 77-yr change was small (1.2-2.1 d) and did not significantly increase early-flowering risk from late-spring/early-summer frost damage.•
Modeled trends in phenological advancement and sensitivity for three northeastern alpine species are less pronounced compared with lower elevations in the region, and this small shift in flower timing did not increase risk of frost damage. Potential reasons for limited earlier phenological advancement at higher elevations include a slower warming trend and increased cloud exposure with elevation and/or inadequate chilling requirements.
研究前提:美国东北部的大多数高山植物是多年生植物,在生长季节早期开花,以此延长其有限的生长季节。与此同时,它们面临着因晚霜而导致繁殖努力付诸东流的风险。除了新罕布什尔州的华盛顿山(海拔1916米)外,物候和气候数据的匮乏限制了对东北高山花卉物候和春末/初夏霜冻风险长期趋势的量化。
方法:利用靠近华盛顿山长期山顶气象站的12个样地4年(2008 - 2011年)的物候和气温测量数据,建立了美国东北部三种高山物种(拉普兰岩菖蒲、比格洛苔草和越桔)的逻辑物候模型。利用样地水平气温、逻辑物候模型和华盛顿山的气候数据,对重点物种的年度(1935 - 2011年)花卉物候和霜冻损害风险进行了后推预测。
主要结果:以-4℃(拉普兰岩菖蒲和比格洛苔草)和-2℃(越桔)为阈值温度的一年中的天数和气温生长度日数最能预测开花。模拟的历史开花日期趋势显著提前,但77年的变化很小(1.2 - 2.1天),且没有显著增加春末/初夏霜冻损害导致的早花风险。
结论:与该地区较低海拔地区相比,模拟的三种东北高山物种物候提前和敏感性趋势不那么明显,而且开花时间的这种小变化并没有增加霜冻损害的风险。高海拔地区物候提前受限的潜在原因包括变暖趋势较慢、随海拔升高云量增加和/或低温需求不足。