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黄淮地区夏秋节气降水的时空演变与集中特征响应OA

Spatiotemporal evolution and concentration characteristics of precipitation during summer and autumn solar terms under climate change in the Huang-Huai region

中文摘要英文摘要

基于 1961-2024 年黄淮地区 177 个国家气象观测站点逐日降水资料,系统分析了该区域夏、秋两季 12 个节气降水量、降水集中度(precipitation concentration degree,PCD)和集中期(precipitation concentration period,PCP)的时空演变及其相互关系.结果表明:1)1961-2024 年,区域年平均降水量为 620.9 mm,呈弱增加趋势(1.43 mm·(10 a)-1);PCD均值为 0.41,降水在时间上趋于集中(0.004·(10 a)-1);PCP 多出现在小暑节气,PCP 呈提前趋势(-0.84°·(10 a)-1).1961-1992 年,降水减少、PCD下降、PCP 提前,而 1993-2024 年则降水增加、PCD 上升、PCP 延后,这种年代际转折可能与东亚夏季风年代际转型及副高位置变化有关.2)区域降水年内呈单峰分布,65.47%的降水集中于夏至至处暑期间,峰值位于小暑(105.3 mm);节气降水趋势差异显著,夏至增量最大(4.24 mm·(10 a)-1),大暑和立秋减幅最剧,分别为-1.98 和-1.29 mm·(10 a)-1.3)PCD自西南向东北递增,豫西山地或因地形抬升降水相对均匀;胶东半岛则可能受副高边缘及海陆作用影响,降水更为集中.少雨年PCD较高(均值为 0.45),反映降水分布更为集中;多雨年 PCD 较低(均值为 0.39),分布则较为均匀.多雨年 PCP 呈自南向北推进的特征,表现为夏至-小暑-大暑的递进格局,与副高北跳的演变过程一致.4)年际尺度上,PCD与区域年均降水量呈弱负相关,但 95.48%的站点其 PCD与年降水量表现为正相关,揭示了极端降水局地性与区域平均效应的差异.PCP 与区域年均降水量呈微弱正相关.节气尺度上,PCD 随主汛期(小暑-立秋)降水量的增加显著增大;PCP 推迟通常与秋季节气(处暑、白露、秋分、寒露)降水增多显著相关,在 1993-2024 年尤为明显.

Based on daily precipitation records from 177 national meteorological stations in the Huang-Huai re-gion from 1961 to 2024,this study systematically examines the spatiotemporal evolution and interrelationships of precipitation amount,precipitation concentration degree(PCD),and precipitation concentration period(PCP)across 12 summer and autumn solar terms.The main findings are as follows:1)From 1961 to 2024,the regional mean annual precipitation was 620.9 mm,exhibiting a weak upward trend(1.43 mm·(10 a)-1).The multiyear mean PCD was 0.41,indicating increasingly concentrated precipitation(0.004(10 a)-1).The PCP mainly oc-curred during the Minor Heat solar term and showed a tendency toward earlier timing(-0.84°·(10 a)-1).From 1961 to 1992,precipitation,PCD,and PCP all decreased,whereas from 1993 to 2024,precipitation and PCD increased and PCP was delayed.This interdecadal shift may be linked to changes in intensity of the East Asi-an summer monsoon and adjustments in the location of the western Pacific subtropical high.2)Regional precipita-tion exhibited a unimodal intra-annual pattern,with 65.47%of the total precipitation occurring between the Sum-mer Solstice and the End of Heat,peaking during Minor Heat(105.3 mm).Trends during individual solar terms differ markedly:the Summer Solstice experienced the strongest increase(4.24 mm·(10 a)-1),while Major Heat and Beginning of Autumn showed the most pronounced decreases(-1.98 mm·(10 a)-1 and-1.29 mm·(10 a)-1,respectively).3)Spatially,PCD increased from southwest to northeast.Low PCD values in the mountainous regions of western Henan likely reflect the influence of more uniformly distributed orographic pre-cipitation,whereas high values over the Jiaodong Peninsula may be associated with its proximity to the subtropi-cal high and strong land-sea thermal contrasts.In low-precipitation years,PCD values were relatively high(mean 0.45),indicating more concentrated precipitation,while high-precipitation years exhibited lower PCD(mean 0.39).During wet years,PCP advanced progressively from south to north,following the sequence Summer Sol-stice-Minor Heat-Major Heat,consistent with the northward seasonal progression of the subtropical high.4)On an annual scale,PCD exhibited a weak negative correlation with regional mean precipitation,although 95.48%of stations showed positive correlations,highlighting the contrast between local extreme events and regional aver-ages.PCP showed a weak positive correlation with regional annual precipitation.At the solar-term scale,PCD in-creased significantly with precipitation during the main flood season(Minor Heat to Beginning of Autumn).In-creased precipitation during autumn solar terms(End of Heat,White Dew,Autumn Equinox,Cold Dew)was significantly associated with delayed PCP,particularly during 1993-2024.

郭冰芳;张艳红;宋艺迪;万举坤;潘攀;刘雅星

中国气象局河南省农业气象保障与应用技术重点实验室,河南 郑州 450003||河南省气候中心,河南 郑州 450003中国气象局河南省农业气象保障与应用技术重点实验室,河南 郑州 450003||河南省气候中心,河南 郑州 450003中国气象局河南省农业气象保障与应用技术重点实验室,河南 郑州 450003||河南省气候中心,河南 郑州 450003东南大学 吴健雄学院,江苏 南京 211189中国气象局河南省农业气象保障与应用技术重点实验室,河南 郑州 450003||河南省气候中心,河南 郑州 450003中国气象局河南省农业气象保障与应用技术重点实验室,河南 郑州 450003||河南省气候中心,河南 郑州 450003

节气降水集中度降水集中期黄淮地区

solar termsprecipitation concentration degree(PCD)precipitation concentration period(PCP)Huang-Huai region

《大气科学学报》 2026 (2)

297-310,14

河南省科技攻关项目(252102320013242102320021)中国气象局河南省农业气象保障与应用技术重点实验室应用技术研究基金项目(KL202405KQ202604)国家自然科学基金区域联合重点项目(U24A20515)江苏省杰出青年基金项目(BK20240036)

10.13878/j.cnki.dqkxxb.20250909001

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