黄河龙头水库多水月(季)预测的地气图方法

英文篇名：Runoff Prediction of the Longyang Gorge Reservoir from Monthly to Seasonal Time Scales Based on the "Di-Qi-Tu" Method
中文刊名：高原气象
英文刊名：Plateau Meteorology
作者：马占良 ; 汤懋苍 ; 雍晓春
英文作者：MA Zhan-liang1 ; TANG Mao-cang2 ; YONG Xiao-chun2 (1.Climate Center of Qinghai Meteorological Bureau ; Xining ; 810001 ; China ; 2.Key Laboratory of Land Sanface Process and Climate Change in Cold and Arid Rigions ; Cold and Arid Regions Environmental and Engineering Research Institute ; Chinese Academy of Sciences ; Lanzhou 730000 ; China)
中文关键词：水库多水期 ; 地气图方法 ; 月(季)预测 ; 东亚强地震 ; 黄河源区
英文关键词：Abundant runoff period ; "Diqi" method ; Monthly seasonal prediction ; Strong earthquake in East Asia ; Source region of Yellow River
出版日期：2010-08-15
机构：青海省气候中心;中国科学院寒区旱区环境与工程研究所寒旱区陆面过程与气候变化重点实验室;
年：2010
期：04
出版单位：高原气象

摘要

利用黄河龙头水库流量控制站——唐乃亥水文站1956年以来逐月流量资料和东亚地震资料及黄河产流区久治气象站1975年以来逐月3.2m地温资料,研究了唐乃亥多水期(流量正距平)的成因及其预报。发现东亚6.5级以上强震形成的地热涡经过黄河源区是唐乃亥多水的原因,具体可分为(1)上游强震涡东移;(2)南北地震带中段强震涡北移;(3)西北太平洋强震涡西退;(4)北方强震的"拍频"作用引发地热涡生成。另外,久治站3.2m地温的增暖过程可作为唐乃亥流量增加的指标。
The causes and predictive method of the abundant runoff at Tang-Nai-Hai hydrological station are discussed based on the monthly runoff data since 1956,a baseline in the upper reach of Yellow River,earthquake records in the East Asia,and the monthly soil temperature data of the Jiuzhi station at 3.2 m since 1975.The results show that the abundant runoff at the Tang-Nai-Hai station is closely related to the geothermal vortex in the original region of Yellow River accompanied by the strong earthquake (Ms≥6.5) in East Asia,they are divided: (1)Eastward movement of the geothermal vortex from the upper reach of Yellow River;(2) Nothward movement of the geothermal vortex from the central part of the north-south earthquake belt;(3) Westward movement of the geothermal vortex from the Northwest Pacific;(4) Enhancement of the geothermal vortex due to the strong earthquake in the north of China.In addition,the increase of 3.2 m soil temperatures at Jiuzhi station is also regarded as a reliable signal of the upcoming increase of the runoff at Tang-Nai-Hai station.

引文

[1]汤懋苍,蔡英,王冬梅.龙羊峡水库入库流量预报的若干问题[M].灾害性气候与农业和水资源.北京:气象出版社,1996:75-80.
    [2]唐红玉,汤懋苍,赵燕宁.龙羊峡入库流量变化的地下原因和预测方法探讨[J].高原气象,2004,23(4):472-475.
    [3]时兴合,张国胜,李林,等.青藏高原大气降水变化规律及其对黄河上游地区水资源的影响[J].气候与环境研究,2000,5(2):195-200.
    [4]汤懋苍,惠小英,郭维栋,等.强地震前的“干热异常”与地温降水波及应变弱停[J].西北地震学报,2010,32(1):99-104.
    [5]赵红岩,汤懋苍,张拥军,等.冬季亚洲强震与夏季我国主雨带的准同纬性[J].地球物理学报,2006,49(3):766-711.
    [6]吴红,汤懋苍,邵志红,等.兰州地温、降水资料对“正多负少规则”的检验[J].高原气象,2009,28(3):581-585.
    [7]汤懋苍.地球系统10-1年变化原因概述[J].高原气象,2009,28(6):1485-1489.
    [8]高晓清,汤懋苍,郭维栋,等.西北太平洋MS≥7.8级强震影响我国月季降水场的过程分析[J].地球物理学报,2008,51(4):1022-1028.
    [9]汤懋苍,赵红岩,张存杰,等.地气图预测气候变化的原理和方法(下)[M].北京:气象出版社(待出版).
    [10]汤懋苍.短期气候预测探索的新方向和新方法[C].中国寒区旱区环境与工程科学50年.北京:科学出版社,2009:320-323.
    [11]汤懋苍,成青燕,张东方,等.地气图预测全国月降水的实践总结[J].高原气象,2008,27(5):1054-1059.
    [12]成青燕,汤懋苍,赵红岩.旱灾的地气形势分类[J].高原气象,2009,28(6):1490-1497.