试析刘宋统治区的气候波动与水旱灾害

J4 ›› 2005, Vol. 23 ›› Issue (4): 66-72.

试析刘宋统治区的气候波动与水旱灾害

刘继宪

郑州大学历史学院，河南郑州450001

收稿日期:2005-05-09 修回日期:2005-11-22 出版日期:2005-12-31 发布日期:2005-12-31
作者简介:刘继宪(1977一)男，山东菏泽人，郑州大学历史学院在读硕士，中国古代史专业.E-mail: Liujixiua@Mail.china. com

Analysis on Climate Fluctuation and Floods and Droughts in Liusong Region

LIU Ji-Xian

School of History Zhen}zhou University Zhen}zhou 450001，China

Received:2005-05-09 Revised:2005-11-22 Online:2005-12-31 Published:2005-12-31

摘要/Abstract

摘要：

刘宋时期虽然整体上属于历史气候变迁中的寒冷期，不过期间存在气温的波动。刘宋初年气温较低，元嘉中后期升至波峰，泰始年间降至波谷，刘宋末年气温再度升高。这种波动通过当时的各种气候资料表现出来，同时也反映在当时的水旱灾害发生特点上。一般在寒冷期，水灾发生的时间要晚，反之，则早。刘宋时期梅雨期到来的早晚和降水量的多少，受制于这种气候波动，同时也影响到当时水旱灾害的发生状况，是这种气温波动的集中表现。

关键词: 气温, 波动, 水旱灾害

Abstract:

Liusong dynasty belongs to the(old period of historical(limate evolution on the whole } but there was a fluctuation of temperature during this period the temperature was relatively low during the early years and during the middle and later periods of Yuanjia,it rose to the highest and dropped to the lowest in the period of Taishi} but in the end of Liusong dynasty the temperature rose again This kind of fluctuation presented through various kinds of(limatic; description is also reflected by the characteristicof floods and droughts at that time. Generally speaking incold period . the time occurging floods in a year is later than that in warm period. The time and precipitation of Meiyu were controlled by the fluc;tuation} and it would influence the(ondition of floods and droughts this is the(onc;entrated expression of temperature fluctuation

Key words: temperature, fluctuation, floods and droughts

中图分类号:

P467

刘继宪. 试析刘宋统治区的气候波动与水旱灾害[J]. J4, 2005, 23(4): 66-72.

LIU Ji-Xian. Analysis on Climate Fluctuation and Floods and Droughts in Liusong Region[J]. J4, 2005, 23(4): 66-72.

[1]	殷宁潞, 李俊林, 洪也, 郭勇, 王式功. 辽宁省两县域城市气温对呼吸系统疾病住院人数的影响[J]. 干旱气象, 2023, 41(1): 132-142.
[2]	冯良敏, 周秋雪, 曹萍萍, 王佳津. 四川地区气温转折过程2 m温度变化订正研究[J]. 干旱气象, 2023, 41(1): 164-172.
[3]	刘蕾, 李鸾, 张丽, 孙大兵, 张晓忆. 1880—2020年安徽芜湖气温长序列构建及年代际特征[J]. 干旱气象, 2022, 40(5): 831-839.
[4]	陈笑晨, 唐振飞, 陈锡宽, 郑潮宇, 李欣欣, 杨婷. 基于CMIP6的福建省极端气温预估[J]. 干旱气象, 2022, 40(3): 415-423.
[5]	张国宏. 秋季巴伦支海海冰与中国京津冀地区2月气温变化的联系[J]. 干旱气象, 2022, 40(2): 187-194.
[6]	陈颖, 贾孜拉·拜山, 邵伟玲, 刘精. 增暖背景下北极涛动对新疆冬季平均气温的影响[J]. 干旱气象, 2022, 40(2): 195-201.
[7]	陈颖, 张冬峰, 王林, 刘月丽, 王大勇. RegCM4对华北区域21世纪气候变化预估研究[J]. 干旱气象, 2022, 40(1): 1-10.
[8]	王丹, 戴昌明, 娄盼星, 王建鹏. 陕西ECMWF、GRAPES_Meso和SCMOC气温预报的对比检验及订正[J]. 干旱气象, 2021, 39(4): 697-708.
[9]	易雪, 杨森, 刘鸣彦, 李涛, 侯依玲, 崔妍. 辽宁省植被覆盖度时空变化特征及其对气候变化的响应[J]. 干旱气象, 2021, 39(2): 252-261.
[10]	徐静, 刘华悦, 靳甜甜, 孙子媛, 付桂琴. 气温对秦皇岛市儿童呼吸系统疾病的影响[J]. 干旱气象, 2021, 39(2): 326-332.
[11]	张建军, 张剑明, 赵新宇, 廖玉芳, 范嘉智. 秋季北极海冰变化对长江中下游地区冬季气温的影响[J]. 干旱气象, 2021, 39(1): 8-14.
[12]	舒建川, 蒋兴文, 宋云帆. 西南冬季气温的年际变化及影响因子分析[J]. 干旱气象, 2021, 39(1): 15-27.
[13]	冯晓莉, 多杰卓么, 李万志, 申红艳, 陈冀青. 1961—2018年青海高原极端气温指数时空变化特征[J]. 干旱气象, 2021, 39(1): 28-37.
[14]	高娜, 孙健, 高睿娜, 王素艳. 气候变化背景下宁夏冬季气温月尺度变化特征[J]. 干旱气象, 2021, 39(1): 38-45.
[15]	肖瑶, 杜明哲, 徐鹏, . 两种订正方法在河南高速公路沿线气温精细化预报中的应用[J]. 干旱气象, 2020, 38(6): 1023-1030.