青藏高原臭氧谷极端事件的定义及其特征
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摘要
利用1979—2016年ERA-interim逐日再分析资料,定义了青藏高原臭氧谷(Ozone Valley over the Tibetan Plateau,OVTP)极端和普通强(弱)事件,并讨论了其特征。结果表明:1) OVTP极端强事件在夏秋季节多发,10月最多,频率达2. 0%; OVTP普通强事件在春夏季多发,7月最多,频率达1. 7%。OVTP极端弱事件在秋冬季多发,12月最多,频率达3. 8%; OVTP普通弱事件在冬季多发,1月最多,频率达2. 0%。2) OVTP极端强事件出现频率显著增加(0. 004%·a~(-1)),极端弱事件出现频率显著减少(-0. 015%·a~(-1))。OVTP普通事件的变化均不显著。3) OVTP极端强事件的面积和强度均在秋季最大,10月达到最大值,面积为4. 3×10~5km~2,强度为1. 5×10~5t; OVTP普通强事件的面积和强度均在夏季最大,7月达到峰值,面积为1. 7×105km~2,强度为4. 1×10~3t。OVTP极端弱事件的面积和强度在春夏较小,4月达到最小值,面积为3. 2×10~4km~2,强度为1. 1×10~2t; OVTP普通弱事件的面积和强度在春夏秋均较小,4月和10月达到极小值,4月面积为2. 5×10~4km~2,强度为68 t,10月面积为2. 2×10~4km~2,强度为97t。4) OVTP极端和普通强事件的面积(强度)均呈显著增大(增强)趋势,极端强事件的面积达2. 5×10~2km~2·a~(-1),强度达2. 5×10~2t·a~(-1),普通强事件的面积达4. 5×10~2km~2·a~(-1),强度达4. 5 t·a~(-1)。极端和普通弱事件的面积(强度)均呈显著减小(减弱)趋势,极端弱事件的面积达-1. 7×10~4km~2·a~(-1),强度达-7. 0×10~3t·a~(-1),普通弱事件的面积达-2. 3×10~3km~2·a~(-1),强度达-2. 7×102t·a~(-1)。
Studies on the extreme events of ozone depletion in the polar region are many but studies on the ozone extreme events of ozone valley over the Tibetan Plateau( OVTP) are few and mainly focus on case analysis.Therefore,this paper defined the extreme and ordinary events of OVTP and analyzed their characteristics based on the ERA-interim daily reanalysis data from 1979 to 2016.Firstly, this paper selected the characteristic isolines of extreme(ordinary) strong and weak OVTP according to total column ozone( TCO) and zonal deviation of TCO( TCO*) after plus or minus 1. 96( 1. 29) standard deviation of TCO and TCO*, respectively. Secondly, this paper defined the extreme strong OVTP with TCO≤250 DU and TCO* ≤-55 DU, the ordinary strong OVTP with 250 DU
Studies on the extreme events of ozone depletion in the polar region are many but studies on the ozone extreme events of ozone valley over the Tibetan Plateau( OVTP) are few and mainly focus on case analysis.Therefore,this paper defined the extreme and ordinary events of OVTP and analyzed their characteristics based on the ERA-interim daily reanalysis data from 1979 to 2016.Firstly, this paper selected the characteristic isolines of extreme(ordinary) strong and weak OVTP according to total column ozone( TCO) and zonal deviation of TCO( TCO*) after plus or minus 1. 96( 1. 29) standard deviation of TCO and TCO*, respectively. Secondly, this paper defined the extreme strong OVTP with TCO≤250 DU and TCO* ≤-55 DU, the ordinary strong OVTP with 250 DU
引文
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刘年庆,黄富祥,王维和,2011.2011年春季北极地区臭氧低值事件的卫星遥感监测[J].科学通报,56(27):2315-2318.Liu N Q,Huang F X,Wang W H,2011.Satellite remote-sensing monitoring ozone low events in the Arctic region in 2011 spring[J].Chin Sci Bull,56(27):2315-2318.(in Chinese).
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陆晏,郭栋,陶丽,等,2017.太阳准周期变化对北半球夏季平流层加热率的影响[J].大气科学学报,40(6):729-736.Lu Y,Guo D,Tao L,et al.,2017.Influence of solar quasi-periodic variation on stratospheric heating rate in the Northern Hemisphere in summer[J].Trans Atmos Sci,40(6):729-736.(in Chinese).
吕达仁,卞建春,陈洪滨,等,2009.平流层大气过程研究的前沿与重要性[J].地球科学进展,24(3):221-228.Lyu D R,Bian J C,Chen H B,et al.,2009.Frontiers and significance of research on stratospheric processes[J].Advances in Earth Science,24(3):221-228.(in Chinese).
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覃皓,郭栋,施春华,等,2018.南亚高压与邻近地区臭氧变化的相互作用[J].大气科学,42(2):421-434.Qin H,Guo D,Shi C H,et al.,2018.The interaction between variations of South Asia High and ozone in the adjacent regions[J].Chin J Atmos Sci,42(2):421-434.(in Chinese).
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