A warm-season drought reconstruction in central-northern Pakistan inferred from tree rings since 1670 CE and its possible climatic mechanism

IF 4.8 2区 环境科学与生态学 Q1 ENVIRONMENTAL SCIENCES Climatic Change Pub Date : 2024-02-15 DOI:10.1007/s10584-024-03688-4
Adam Khan, Feng Chen, Heli Zhang, Sidra Saleem, Hamada E. Ali, Weipeng Yue, Martín Hadad
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Abstract

Understanding past warm-season drought variability and its underlying climatic mechanisms is crucial for effective drought management and climate adaptation strategies. In this study, we develop a regional chronology (RC) spanning from 1620 to 2017 CE by utilizing dendrochronological techniques and tree-ring data from two stands of Abies pindrow. The RC reveals a significant positive correlation (p < 0.05) with self-calibrated Palmer drought severity index (scPDSI) and precipitation and a significant negative correlation with temperature. We use a simple linear regression model between RC and climate data to reconstruct a 348-year-long (1670–2017 CE) warm-season (April-July) drought variability from central-northern Pakistan. The reconstructed scPDSI reveals a 44% variance of the scPDSI during the common calibrated period 1950–2017 CE. Spatial correlation shows a positive field correlation with central-northern Pakistan, extending predominantly to neighboring regions. MTM (multi-taper method) spectral analysis reveals inter-annual cycles (6.8, 3.2, 2.7, 2.5, and 2.3 years) and multi-decadal cycles (11.7, 15.2, 16.2, 17.9, and 128 years). The internal-annual cycles demonstrate a possible linkage between reconstructed scPDSI and El Niño–Southern Oscillation (ENSO). The reconstructed scPDSI agrees well with the moisture-sensitive tree-ring records from northern Pakistan and neighboring regions. Our reconstruction shows a significant correlation with the South Asia Summer Monsoon Index (SASMI), Atlantic Multi-decadal Oscillation (AMO), ENSO, Pacific Decadal Oscillation (PDO), and solar activity, emphasizing that all these factors have some influence on the drought variability in central-northern Pakistan. This study has important implications for disaster management and proactive measures for mitigating the impact of drought on both natural ecosystems and human populations in central-northern Pakistan and associated regions.

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根据西元 1670 年以来的树木年轮推断的巴基斯坦中北部暖季干旱重建及其可能的气候机制
了解过去暖季干旱的变异性及其潜在的气候机制对于有效的干旱管理和气候适应战略至关重要。在这项研究中,我们利用树木年代学技术和来自两个松柏林的树环数据,建立了从公元 1620 年到 2017 年的区域年表(RC)。该年表与自校准帕尔默干旱严重程度指数(scPDSI)和降水量呈显著正相关(p < 0.05),与温度呈显著负相关。我们利用 RC 与气候数据之间的简单线性回归模型,重建了巴基斯坦中北部长达 348 年(西元 1670 年至 2017 年)的暖季(4 月至 7 月)干旱变率。重建的 scPDSI 显示,在 1950-2017 CE 共同校准期间,scPDSI 的变率为 44%。空间相关性显示与巴基斯坦中北部存在正的实地相关性,主要延伸至邻近地区。MTM(多锥度法)光谱分析显示了年际周期(6.8、3.2、2.7、2.5 和 2.3 年)和多年周期(11.7、15.2、16.2、17.9 和 128 年)。内部年周期表明重建的 scPDSI 与厄尔尼诺-南方涛动(ENSO)之间可能存在联系。重建的 scPDSI 与巴基斯坦北部及邻近地区的湿度敏感树环记录非常吻合。我们的重建结果显示了与南亚夏季季风指数(SASMI)、大西洋十年期涛动(AMO)、厄尔尼诺-南方涛动(ENSO)、太平洋十年期涛动(PDO)和太阳活动的显著相关性,强调了所有这些因素都对巴基斯坦中北部的干旱变化有一定影响。这项研究对于灾害管理和采取积极措施减轻干旱对巴基斯坦中北部及相关地区自然生态系统和人口的影响具有重要意义。
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来源期刊
Climatic Change
Climatic Change 环境科学-环境科学
CiteScore
10.20
自引率
4.20%
发文量
180
审稿时长
7.5 months
期刊介绍: Climatic Change is dedicated to the totality of the problem of climatic variability and change - its descriptions, causes, implications and interactions among these. The purpose of the journal is to provide a means of exchange among those working in different disciplines on problems related to climatic variations. This means that authors have an opportunity to communicate the essence of their studies to people in other climate-related disciplines and to interested non-disciplinarians, as well as to report on research in which the originality is in the combinations of (not necessarily original) work from several disciplines. The journal also includes vigorous editorial and book review sections.
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