气象与环境学报
氣象與環境學報
기상여배경학보
JOURNAL OF METEOROLOGY AND ENVIRONMENT
2012年
4期
22-27
,共6页
高峰%姚国友%朱晓飞%涂钢%隋波
高峰%姚國友%硃曉飛%塗鋼%隋波
고봉%요국우%주효비%도강%수파
采暖期%气温%采暖指数%采暖强度%能源消耗
採暖期%氣溫%採暖指數%採暖彊度%能源消耗
채난기%기온%채난지수%채난강도%능원소모
Heating period%Air temperature%Heating index%Heating intensity%Energy consumption
利用1960—2009年吉林省46个测站平均气温和最低气温资料,利用采暖强度、采暖指数、气温趋势倾向和M-K检验方法,分析吉林省采暖期气温变化特征及变化规律。结果表明:吉林省采暖期平均气温、最低气温均呈上升趋势,低于-20℃的日数明显减少。近50 a平均气温、最低气温趋势倾向值为0.24℃/10 a、0.42℃/10 a;特别是近10 a来上升趋势明显,平均气温、最低气温倾向值为0.84℃/10 a、1.25℃/10 a,最低气温的升温趋势较为明显。吉林省采暖开始日呈推迟趋势,采暖结束日呈提前趋势,从而使采暖期日数缩短。根据突变分析,采暖期气温变化的突变年为1985年。吉林省采暖期长、采暖强度强的年份大部分出现在20世纪80年代中期以前;采暖期短、采暖强度弱的年份多出现在80年代以后。采暖指数分析表明,20世纪80年代中期以前,采暖指数以正值为主;80年代中期以后,采暖指数以负值为主,90年代均为负值,但在近10 a采暖指数波动幅度加大。由于采暖强度降低、采暖期日数缩短,合理利用气温条件开展采暖工作,可以减少向大气排放CO2、SO2和NO2,对减缓气候变暖、改善大气环境质量有重要的现实意义。
利用1960—2009年吉林省46箇測站平均氣溫和最低氣溫資料,利用採暖彊度、採暖指數、氣溫趨勢傾嚮和M-K檢驗方法,分析吉林省採暖期氣溫變化特徵及變化規律。結果錶明:吉林省採暖期平均氣溫、最低氣溫均呈上升趨勢,低于-20℃的日數明顯減少。近50 a平均氣溫、最低氣溫趨勢傾嚮值為0.24℃/10 a、0.42℃/10 a;特彆是近10 a來上升趨勢明顯,平均氣溫、最低氣溫傾嚮值為0.84℃/10 a、1.25℃/10 a,最低氣溫的升溫趨勢較為明顯。吉林省採暖開始日呈推遲趨勢,採暖結束日呈提前趨勢,從而使採暖期日數縮短。根據突變分析,採暖期氣溫變化的突變年為1985年。吉林省採暖期長、採暖彊度彊的年份大部分齣現在20世紀80年代中期以前;採暖期短、採暖彊度弱的年份多齣現在80年代以後。採暖指數分析錶明,20世紀80年代中期以前,採暖指數以正值為主;80年代中期以後,採暖指數以負值為主,90年代均為負值,但在近10 a採暖指數波動幅度加大。由于採暖彊度降低、採暖期日數縮短,閤理利用氣溫條件開展採暖工作,可以減少嚮大氣排放CO2、SO2和NO2,對減緩氣候變暖、改善大氣環境質量有重要的現實意義。
이용1960—2009년길림성46개측참평균기온화최저기온자료,이용채난강도、채난지수、기온추세경향화M-K검험방법,분석길림성채난기기온변화특정급변화규률。결과표명:길림성채난기평균기온、최저기온균정상승추세,저우-20℃적일수명현감소。근50 a평균기온、최저기온추세경향치위0.24℃/10 a、0.42℃/10 a;특별시근10 a래상승추세명현,평균기온、최저기온경향치위0.84℃/10 a、1.25℃/10 a,최저기온적승온추세교위명현。길림성채난개시일정추지추세,채난결속일정제전추세,종이사채난기일수축단。근거돌변분석,채난기기온변화적돌변년위1985년。길림성채난기장、채난강도강적년빈대부분출현재20세기80년대중기이전;채난기단、채난강도약적년빈다출현재80년대이후。채난지수분석표명,20세기80년대중기이전,채난지수이정치위주;80년대중기이후,채난지수이부치위주,90년대균위부치,단재근10 a채난지수파동폭도가대。유우채난강도강저、채난기일수축단,합리이용기온조건개전채난공작,가이감소향대기배방CO2、SO2화NO2,대감완기후변난、개선대기배경질량유중요적현실의의。
Based on the mean temperature,the minimum temperature data from 46 weather stations from 1960 to 2009 in Jilin province,heating intensity and heating index were calculated,and the characteristics of temperature variation and rules were analyzed by methods of a tendency analysis and a Mann-Kendall test.The results indicate that the mean and minimum temperatures are the increasing trends in the heating period.The number of days that temperature is lower than-20 ℃ decreases obviously.The mean and minimum temperature tendency rates are 0.24 ℃/decade and 0.42 ℃/decade in the recent 50 years,especially in the recent decade with 0.84 ℃/decade and 1.25 ℃/decade respectively,and the increasing tendency of the minimum temperature is obvious.The heating beginning date is in a delaying trend,while the heating ending date is in an advancing trend.Thus,the number of days of the heating period is shortened.The abrupt change of temperature during the heating period occurs in 1985.The heating period is long and the heating intensity is strong before the middle period of 1980s,while the heating period is short and the heating intensity is weak after 1980s.The heating index is mainly positive before the middle period of 1980s,while it is mainly negative after 1980s,especially in 1990s.However,the fluctuant amplitude of the heating index increases in the recent decade.The reasonable heating plans could be carried out according to temperature conditions because of the decreasing heating intensity and the shortening heating days,which can reduce emissions of carbon dioxide,sulfur dioxide and nitrogen dioxide to the atmosphere and it is important to palliation climate warming and improve the quality of atmospheric environment.