模拟高温干旱对得克萨斯州森林的影响

Shakirudeen Lawal, Jennifer Costanza, Frank H. Koch, Robert M. Scheller
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引用次数: 0

摘要

在气候变化的影响下,干旱对森林生态系统的影响越来越大,进而对生态系统服务产生影响。2011 年,得克萨斯州发生了历史上罕见的干旱,造成大量树木死亡。我们使用 2004-2019 年森林资源清查与分析 (FIA) 数据和全州天气数据,研究了与树木死亡率升高相关的气候条件。我们使用标准化降水蒸散指数 (SPEI) 以两种时间尺度(12 个月和 36 个月)测量了极端湿度(从湿到干)。在同一时期,我们使用每日热浪强度指数(HWMId)量化热浪的严重程度。我们对德克萨斯州四个地区(东南部、东北部、中北部和南部)的树木死亡率与这些指数之间的关系进行了统计建模,并对主要树属(松属、桧属、柞属、枫属、崖柏属和榆属)以及部分树种进行了统计建模:树木死亡率最高的时期是 2011 年至 2013 年。我们发现 12 个月 SPEI 和 36 个月 SPEI 的趋势具有相似性,两者在 2011 年都表现出比其他年份更极端的负面强度(即干旱)。同样,我们发现 2011 年的极端高温也远高于其他年份。与得克萨斯州中部(即中北部和南部)相比,得克萨斯州东部(即东南部和东北部)的热浪和干旱更为严重。在梯度提升回归模型中,36 个月 SPEI 与树木死亡率的经验关系比 12 个月 SPEI 更密切,但得克萨斯州南部除外,在得克萨斯州南部,HWMId 比 SPEI 在任一时间尺度上的影响都要大。极端湿度、极端高温与树木死亡率之间的相关性很高;通常,死亡率在极端湿度不足而非过剩期间达到峰值,这表明死亡率与高温干旱条件有关。对于除橡树(栎树)以外的所有树属而言,极端高温的影响都大于 SPEI 的影响。除水栎(Q. nigra)以外的其他栎类也是如此。在广义加和模型中,中位数趋势表明,在中度干旱(SPEI36 ∼ -1)或更严重的条件下,红花楹的树木死亡率较高;但在轻度干旱(SPEI36 ∼ -0.5)条件下,松树和栎树的死亡率开始显现。极端高温对杜松死亡率的影响发生在热浪等级达到超极端等级(HWMId > 80)时,但对枫香树的影响则发生在较低等级时。在气候不断变化的情况下,预计类似的风险会更频繁地出现。
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Modeling the impacts of hot drought on forests in Texas
Under climate change, drought is increasingly affecting forest ecosystems, with subsequent consequences for ecosystem services. An historically exceptional drought in Texas during 2011 caused substantial tree mortality. We used 2004–2019 Forest Inventory and Analysis (FIA) data and state-wide weather data to examine the climatic conditions associated with this elevated tree mortality.We measured moisture extremes (wet to dry) using the Standardized Precipitation Evapotranspiration Index (SPEI) at two timescales (12- and 36-month). We quantified heat wave severity using the Heat Wave Magnitude Index daily (HWMId) over the same period. We performed statistical modeling of the relationship between tree mortality and these indices across four Texas regions (Southeast, Northeast, North Central, and South) and for prominent tree genera (Pinus, Juniperus, Quercus, Liquidambar, Prosopis, and Ulmus) as well as selected species: Quercus stellata, Q. virginiana, and Q. nigra.The highest tree mortality was observed between 2011 and 2013. We found similarity in the trends of the 12- and 36-month SPEI, both of which exhibited more extreme negative intensities (i.e., drought) in 2011 than other years. Likewise, we found that the extreme heat experienced in 2011 was much greater than what was experienced in other years. The heat waves and drought were more intense in East (i.e., Southeast and Northeast) Texas than Central (i.e., North Central and South) Texas. In gradient boosted regression models, the 36-month SPEI had a stronger empirical relationship with tree mortality than the 12-month SPEI in all regions except South Texas, where HWMId had more influence than SPEI at either timescale. The correlations between moisture extremes, extreme heat, and tree mortality were high; typically, mortality peaked after periods of extreme moisture deficit rather than surplus, suggesting that the mortality was associated with hot drought conditions. The effects of extreme heat outweighed those of SPEI for all tree genera except oaks (Quercus). This was also true for oak species other than water oak (Q. nigra). In generalized additive models, the median trend showed tree mortality of Prosopis was higher during conditions of moderate drought (SPEI36 ∼ –1) or worse, but for Pinus and Quercus, mortality started to become apparent under mild drought conditions (SPEI36 ∼ –0.5). The impacts of extreme heat on the mortality of Juniperus occurred when heat wave magnitude reached the ultra extreme category (HWMId > 80) but occurred at lower magnitude for Liquidambar.In summary, we identified risks to Texas forest ecosystems from exposure to climate extremes. Similar exposure can be expected to occur more frequently under a changing climate.
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