生态环境学报
生態環境學報
생태배경학보
ECOLOGY AND ENVIRONMENT
2013年
1期
50-57
,共8页
气候变化%植物物候%荒漠化草原%内蒙古
氣候變化%植物物候%荒漠化草原%內矇古
기후변화%식물물후%황막화초원%내몽고
climate change%phenological phase%desert steppe%Inner Mongolia
近年来,植物物候已成为全球变化敏感而准确的综合指示器.深入研究区域气候变化对草原优势牧草生长发育的影响和监测草原生态环境变化,对指导当地农牧业生产、作物品种的生态学分类、自然区划或农业气候区划的指标,提供有力的基础理论支持.文章基于内蒙古西部荒漠化草原乌审召和锡林高勒两个牧业气象试验站1983—2009年优势牧草的物候期数据和同期气象数据,在分析年平均气温、年降水量和牧草物候期各指标线性趋势的基础上,研究了气候变化对内蒙古荒漠化草原优势牧草返青、开花与黄枯日期早晚的影响,结果表明:(1)1983—2007年内蒙古荒漠化草原区年平均气温升高明显,气候倾向率在0.34~0.57℃/10a 之间,年降水量无显著变化,气候朝着暖干化方向发展.(2)受春季气温和降水的影响,27年间内蒙古荒漠化草原区供试草种中,除乌审召的碱茅返青呈现明显的延后趋势,平均每年延后0.6 d外,大部分牧草发育期呈提早趋势,幅度为0.1~0.6 d/a;研究期间,优势牧草的开花期总体呈提早趋势,其中锡林高勒的霸王和猫头刺开花提早最为显著,二者始花日期平均每年提前0.5 d和1.1 d;在夏末初秋气温和降水的综合影响下,内蒙古荒漠化草原区不同站点优势牧草的黄枯期变化差异明显,其中乌审召的优势牧草黄枯均表现为显著或极显著的延后趋势,幅度为0.6 d~0.8 d/a;而锡林高勒优势牧草的黄枯期则大部分表现为不显著的提前态势,究其原因,是由于锡林高勒站点在牧草黄枯前1~2个月气温升高和降水量减少所致.(3)虽然荒漠化草原区各草种物候期均有所变化,但整体上在气候变暖的背景下,所有供试植物生长季均不同程度的延长.
近年來,植物物候已成為全毬變化敏感而準確的綜閤指示器.深入研究區域氣候變化對草原優勢牧草生長髮育的影響和鑑測草原生態環境變化,對指導噹地農牧業生產、作物品種的生態學分類、自然區劃或農業氣候區劃的指標,提供有力的基礎理論支持.文章基于內矇古西部荒漠化草原烏審召和錫林高勒兩箇牧業氣象試驗站1983—2009年優勢牧草的物候期數據和同期氣象數據,在分析年平均氣溫、年降水量和牧草物候期各指標線性趨勢的基礎上,研究瞭氣候變化對內矇古荒漠化草原優勢牧草返青、開花與黃枯日期早晚的影響,結果錶明:(1)1983—2007年內矇古荒漠化草原區年平均氣溫升高明顯,氣候傾嚮率在0.34~0.57℃/10a 之間,年降水量無顯著變化,氣候朝著暖榦化方嚮髮展.(2)受春季氣溫和降水的影響,27年間內矇古荒漠化草原區供試草種中,除烏審召的堿茅返青呈現明顯的延後趨勢,平均每年延後0.6 d外,大部分牧草髮育期呈提早趨勢,幅度為0.1~0.6 d/a;研究期間,優勢牧草的開花期總體呈提早趨勢,其中錫林高勒的霸王和貓頭刺開花提早最為顯著,二者始花日期平均每年提前0.5 d和1.1 d;在夏末初鞦氣溫和降水的綜閤影響下,內矇古荒漠化草原區不同站點優勢牧草的黃枯期變化差異明顯,其中烏審召的優勢牧草黃枯均錶現為顯著或極顯著的延後趨勢,幅度為0.6 d~0.8 d/a;而錫林高勒優勢牧草的黃枯期則大部分錶現為不顯著的提前態勢,究其原因,是由于錫林高勒站點在牧草黃枯前1~2箇月氣溫升高和降水量減少所緻.(3)雖然荒漠化草原區各草種物候期均有所變化,但整體上在氣候變暖的揹景下,所有供試植物生長季均不同程度的延長.
근년래,식물물후이성위전구변화민감이준학적종합지시기.심입연구구역기후변화대초원우세목초생장발육적영향화감측초원생태배경변화,대지도당지농목업생산、작물품충적생태학분류、자연구화혹농업기후구화적지표,제공유력적기출이론지지.문장기우내몽고서부황막화초원오심소화석림고륵량개목업기상시험참1983—2009년우세목초적물후기수거화동기기상수거,재분석년평균기온、년강수량화목초물후기각지표선성추세적기출상,연구료기후변화대내몽고황막화초원우세목초반청、개화여황고일기조만적영향,결과표명:(1)1983—2007년내몽고황막화초원구년평균기온승고명현,기후경향솔재0.34~0.57℃/10a 지간,년강수량무현저변화,기후조착난간화방향발전.(2)수춘계기온화강수적영향,27년간내몽고황막화초원구공시초충중,제오심소적감모반청정현명현적연후추세,평균매년연후0.6 d외,대부분목초발육기정제조추세,폭도위0.1~0.6 d/a;연구기간,우세목초적개화기총체정제조추세,기중석림고륵적패왕화묘두자개화제조최위현저,이자시화일기평균매년제전0.5 d화1.1 d;재하말초추기온화강수적종합영향하,내몽고황막화초원구불동참점우세목초적황고기변화차이명현,기중오심소적우세목초황고균표현위현저혹겁현저적연후추세,폭도위0.6 d~0.8 d/a;이석림고륵우세목초적황고기칙대부분표현위불현저적제전태세,구기원인,시유우석림고륵참점재목초황고전1~2개월기온승고화강수량감소소치.(3)수연황막화초원구각초충물후기균유소변화,단정체상재기후변난적배경하,소유공시식물생장계균불동정도적연장.
Climate change has been an accurate and sensitive indicator of global change in recent years. In order to take the further study on the effects of regional climate change on the plants phenological phase in the desert steppe, monitor the changes of grassland ecological environment, make for crop varieties classification of ecology, natural division of agricultural climate zoning or index, guide the local agriculture and husbandry production, provide the basic theory of strong support, the phenological observation data (the germination date, flowering date, wilting date and growing season length) and corresponding meteorological data from two meteorological stations of the desert steppe in western Inner Mongolia during 1983 to 2009 were used to reveal statistical relationships between phenology and meteorology. The results showed as follows:(1) It showed the ascending trend of annual mean temperature in the desert steppe in Inner Mongolia, the increased rate was about 0.34~0.75℃/10a and the change of precipitation was not apparent. The climate was getting warmer and drier. (2) Most plants′green up dates was intensely affected by mean tempreture and precipitation in spring (from March to May), the dates were 0.1~0.6 d/a in advance except Puccinellia distans L. The flowering periods of the dominant species were also becoming earlier. For instance, flowering dates of Sarcozygium xanthoxylum Bunge and Oxytropis aciphylla Ledeb. in Xilingaole was getting ahead at 0.5 d/a and 1.1 d/a degrees respectively. The wilting date was influenced by the water and heat condition from late summer to early autumn and they were different at two stations. Species withered in Wushenzhao postponed for about 0.6~0.8 d/a while plants turned yellow in Xilingaole had an exhibition of the trend of the advance because the date of withered stage was closely related to precipitation and tempreture prior to withering and yellowing in Xilingaole. (3)With the climate warming, the growing season lengths of all the tested species had prolonged though their phenological phases had changed.