Key Laboratory of Alpine Ecology and Biodiversity, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, 16 Lincui Road, Chaoyang District, 100101, Beijing, China.
CAS Center for Excellence in Tibetan Plateau Earth Sciences, 16 Lincui Road, Chaoyang District, 100101 Beijing, China.
Glob Chang Biol. 2015 Oct;21(10):3647-56. doi: 10.1111/gcb.12961. Epub 2015 Jun 19.
The ongoing changes in vegetation spring phenology in temperate/cold regions are widely attributed to temperature. However, in arid/semiarid ecosystems, the correlation between spring temperature and phenology is much less clear. We test the hypothesis that precipitation plays an important role in the temperature dependency of phenology in arid/semiarid regions. We therefore investigated the influence of preseason precipitation on satellite-derived estimates of starting date of vegetation growing season (SOS) across the Tibetan Plateau (TP). We observed two clear patterns linking precipitation to SOS. First, SOS is more sensitive to interannual variations in preseason precipitation in more arid than in wetter areas. Spatially, an increase in long-term averaged preseason precipitation of 10 mm corresponds to a decrease in the precipitation sensitivity of SOS by about 0.01 day mm(-1) . Second, SOS is more sensitive to variations in preseason temperature in wetter than in dryer areas of the plateau. A spatial increase in precipitation of 10 mm corresponds to an increase in temperature sensitivity of SOS of 0.25 day °C(-1) (0.25 day SOS advance per 1 °C temperature increase). Those two patterns indicate both direct and indirect impacts of precipitation on SOS on TP. This study suggests a balance between maximizing benefit from the limiting climatic resource and minimizing the risk imposed by other factors. In wetter areas, the lower risk of drought allows greater temperature sensitivity of SOS to maximize the thermal benefit, which is further supported by the weaker interannual partial correlation between growing degree days and preseason precipitation. In more arid areas, maximizing the benefit of water requires greater sensitivity of SOS to precipitation, with reduced sensitivity to temperature. This study highlights the impacts of precipitation on SOS in a large cold and arid/semiarid region and suggests that influences of water should be included in SOS module of terrestrial ecosystem models for drylands.
温带/寒带地区植被物候春季变化的持续发生被广泛归因于温度。然而,在干旱/半干旱生态系统中,春季温度与物候之间的相关性则不那么明显。我们检验了一个假设,即在干旱/半干旱地区,降水在物候对温度的依赖性中起着重要作用。因此,我们调查了 preseason降水对青藏高原(TP)植被生长季节开始日期(SOS)卫星估算值的影响。我们观察到两个明显的模式,将降水与 SOS 联系起来。首先,在更干旱的地区,SOS 对 preseason降水的年际变化更为敏感,而在较湿润的地区则不那么敏感。从空间上看,长期平均 preseason降水增加 10 毫米对应于 SOS 对降水敏感性的降低约 0.01 天毫米(-1)。其次,在高原较湿润地区,SOS 对 preseason温度变化更为敏感,而在较干燥地区则不那么敏感。降水增加 10 毫米对应于 SOS 对温度敏感性的增加 0.25 天°C(-1)(每 1°C 温度升高 SOS 提前 0.25 天)。这两种模式表明降水对青藏高原 SOS 的直接和间接影响。本研究表明,在最大限度地利用限制气候资源的好处和最小化其他因素带来的风险之间存在平衡。在较湿润地区,干旱风险较低,允许 SOS 对温度的敏感性更大,以最大限度地提高热量效益,而生长度日与 preseason 降水之间的年际部分相关性较弱进一步支持了这一点。在较干旱地区,最大限度地利用水的好处需要 SOS 对降水的敏感性更大,而对温度的敏感性则降低。本研究强调了降水对大冷带干旱和半干旱地区 SOS 的影响,并建议在旱地陆地生态系统模型的 SOS 模块中纳入水分的影响。