CREAF Cerdanyola del Vallès, Barcelona, Spain.
CTFC, Solsona, Spain.
Glob Chang Biol. 2017 Aug;23(8):3219-3230. doi: 10.1111/gcb.13663. Epub 2017 Mar 22.
Ongoing climate change may undermine the effectiveness of protected area networks in preserving the set of biotic components and ecological processes they harbor, thereby jeopardizing their conservation capacity into the future. Metrics of climate change, particularly rates and spatial patterns of climatic alteration, can help assess potential threats. Here, we perform a continent-wide climate change vulnerability assessment whereby we compare the baseline climate of the protected area network in North America (Canada, United States, México-NAM) to the projected end-of-century climate (2071-2100). We estimated the projected pace at which climatic conditions may redistribute across NAM (i.e., climate velocity), and identified future nearest climate analogs to quantify patterns of climate relocation within, among, and outside protected areas. Also, we interpret climatic relocation patterns in terms of associated land-cover types. Our analysis suggests that the conservation capacity of the NAM protection network is likely to be severely compromised by a changing climate. The majority of protected areas (~80%) might be exposed to high rates of climate displacement that could promote important shifts in species abundance or distribution. A small fraction of protected areas (<10%) could be critical for future conservation plans, as they will host climates that represent analogs of conditions currently characterizing almost a fifth of the protected areas across NAM. However, the majority of nearest climatic analogs for protected areas are in nonprotected locations. Therefore, unprotected landscapes could pose additional threats, beyond climate forcing itself, as sensitive biota may have to migrate farther than what is prescribed by the climate velocity to reach a protected area destination. To mitigate future threats to the conservation capacity of the NAM protected area network, conservation plans will need to capitalize on opportunities provided by the existing availability of natural land-cover types outside the current network of NAM protected areas.
持续的气候变化可能会降低保护区网络保护其所容纳的生物组成部分和生态过程的有效性,从而危及它们未来的保护能力。气候变化的指标,特别是气候变化的速度和空间模式,可以帮助评估潜在的威胁。在这里,我们进行了一次全大陆范围的气候变化脆弱性评估,将北美的保护区网络的基线气候(加拿大、美国、墨西哥-北美)与本世纪末的预测气候(2071-2100 年)进行了比较。我们估计了气候条件可能在北美范围内重新分布的速度(即气候速度),并确定了未来最近的气候类似物,以量化保护区内、保护区之间和保护区外的气候迁移模式。此外,我们根据相关的土地覆盖类型来解释气候迁移模式。我们的分析表明,气候变化可能严重影响北美保护网络的保护能力。约 80%的保护区可能面临高气候位移率,这可能会导致物种丰度或分布的重要变化。一小部分保护区(<10%)可能对未来的保护计划至关重要,因为它们将拥有目前几乎占北美保护区面积五分之一的条件的类似气候。然而,大多数保护区的最近气候类似物都在非保护区。因此,除了气候压力本身之外,未受保护的景观可能会构成额外的威胁,因为敏感的生物群可能不得不迁移到比气候速度规定的更远的地方,才能到达保护区目的地。为了减轻未来对北美保护区网络保护能力的威胁,保护计划将需要利用现有非保护区自然土地覆盖类型的可用性提供的机会。