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Legacies of La Nina: North American monsoon can rescue trees from winter drought

机译:La Nina的遗产:北美季风可以从冬季干旱中拯救树木

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While we often assume tree growth-climate relationships are time-invariant, impacts of climate phenomena such as the El Nino Southern Oscillation (ENSO) and the North American Monsoon (NAM) may challenge this assumption. To test this assumption, we grouped ring widths (1900-present) in three southwestern US conifers into La Nina periods (LNP) and other years (OY). The 4 years following each La Nina year are included in LNP, and despite 1-2 year growth declines, compensatory adjustments in tree growth responses result in essentially equal mean growth in LNP and OY, as average growth exceeds OY means 2-4 years after La Nina events. We found this arises because growth responses in the two periods are not interchangeable: Due to differences in growth-climate sensitivities and climatic memory, parameters representing LNP growth fail to predict OY growth and vice versa (decreases in R-2 up to 0.63; lowest R-2 = 0.06). Temporal relationships between growth and antecedent climate (memory) show warmer springs and longer growing seasons negatively impact growth following dry La Nina winters, but that NAM moisture can rescue trees after these events. Increased importance of monsoonal precipitation during LNP is key, as the largest La Nina-related precipitation deficits and monsoonal precipitation contributions both occur in the southern part of the region. Decreases in first order autocorrelation during LNP were largest in the heart of the monsoon region, reflecting both the greatest initial growth declines and the largest recovery. Understanding the unique climatic controls on growth in Southwest conifers requires consideration of both the influences and interactions of drought, ENSO, and NAM, each of which is likely to change with continued warming. While plasticity of growth sensitivity and memory has allowed relatively quick recovery in the tree-ring record, recent widespread mortality events suggest conditions may soon exceed the capacity for adjustment in current populations.
机译:虽然我们经常假设树木生长气候关系是时间不变的,但气候现象的影响,如El Nino Southern振荡(ENSO)和北美季风(NAM)可能会挑战这种假设。为了测试这一假设,我们将三个西南美国针叶树分组为La Nina(LNP)和其他年份(OY)。每年4岁以下都包含在LNP中,尽管增长1-2岁,但树木增长应对的补偿调整导致LNP和OY基本相等的平均增长,随着平均增长超过OY意味着2 - 4年La Nina活动。我们发现这一点是因为两个时期的生长反应不可互换:由于生长气候敏感性和气候记忆的差异,代表LNP增长的参数未能预测OY的生长,反之亦然(R-2的降低高达0.63;最低R-2 = 0.06)。增长和前一种气候(记忆)之间的时间关系显示较温暖的弹簧和更长的生长季节在Dry La Nina Winters之后产生负面影响,但Nam水分可以在这些事件后救援树木。由于最大的LA NINA相关的降水缺陷和季风降水缺陷,因此在该地区的南部发生,季风降水的重要性增加。在LNP期间,在季风区的心脏中最大的第一顺序自相关减少,反映了最大的初始增长下降和最大的恢复。了解西南针叶树的生长的独特气候控制需要考虑干旱,ENSO和NAM的影响和相互作用,每个人都可能随着持续变暖而变化。虽然生长敏感性和记忆的可塑性在树木记录中允许相对快速地康复,但最近的广泛死亡率事件表明条件可能很快可能超越当前人口调整的能力。

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