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首页> 外文期刊>Atmospheric chemistry and physics >Observations and analysis of polar stratospheric clouds detected by POAM III and SAGE III during the SOLVE II/VINTERSOL campaign in the 2002/2003 Northern Hemisphere winter
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Observations and analysis of polar stratospheric clouds detected by POAM III and SAGE III during the SOLVE II/VINTERSOL campaign in the 2002/2003 Northern Hemisphere winter

机译:在2002/2003年北半球冬季SOLVE II / VINTERSOL运动中,POAM III和SAGE III探测到的极地平流层云的观测和分析

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The Polar Ozone and Aerosol Measurement and Stratospheric Aerosol and GasExperiment instruments both observed high numbers of polar stratosphericclouds (PSCs) in the polar region during the second SAGE Ozone Loss andValidation (SOLVE II) and Validation of INTERnational Satellites and Studyof Ozone Loss (VINTERSOL) campaign, conducted during the 2002/2003 NorthernHemisphere winter. Between 15 November 2002 (14 November 2002) and 18 March2003 (21 March 2003) SAGE (POAM) observed 122 (151) aerosol extinctionprofiles containing PSCs. PSCs were observed on an almost daily basis, fromearly December through 15 January, in both instruments. No PSCs wereobserved from either instrument from 15 January until 4 February, and fromthen only sparingly in three periods in mid- and late February and mid-March.In early December, PSCs were observed in the potential temperature rangefrom roughly 375 K to 750 K. Throughout December the top of this rangedecreases to near 600 K. In February and March, PSC observations wereprimarily constrained to potential temperatures below 500 K. The PSCobservation frequency as a function of ambient temperature relative to thenitric acid-trihydrate saturation point (using a nitric acid profile priorto denitrification) was used to infer irreversible denitrification. By lateDecember 38% denitrification was inferred at both the 400–475 K and475–550 K potential temperature ranges. By early January extensive levels ofdenitrification near 80% were inferred at both potential temperatureranges, and the air remained denitrified at least through early March.
机译:极地臭氧和气溶胶测量以及平流层气溶胶和GasExperiment仪器都在第二次SAGE臭氧损失和验证(SOLVE II)以及国际卫星验证和臭氧损失研究(VINTERSOL)活动期间,在极地观测到大量极地平流层云(PSC)。 ,在2002/2003年北半球冬季进行。在2002年11月15日(2002年11月14日)和2003年3月18日(2003年3月21日)之间,SAGE(POAM)观测到122(151)个含有PSC的气溶胶消光剖面。从12月上旬至1月15日几乎每天都在这两种仪器中观察到PSC。从1月15日至2月4日,从这两种仪器中均未观察到PSC,然后从2月中下旬至3月中的三个时段中很少观察到PSC.12月初,在大约375 K至750 K的潜在温度范围内观察到了PSC。整个12月,该范围的顶部减小到接近600K。在2月和3月,PSC观测主要被限制在低于500 K的潜在温度下。PSC观测频率是环境温度相对于硝酸三水合物饱和点的函数(使用硝酸(反硝化之前的温度分布)来推断不可逆的反硝化作用。到12月下旬,推断在400–475 K和475–550 K的潜在温度范围内的反硝化作用为38%。到1月初,在两个可能的温度范围内都可以推断出接近80%的广泛的反硝化作用,并且至少到3月初,空气仍保持着反硝化状态。

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