首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >Monthly mean vertical profiles of pressure, temperature and water vapour volume mixing ratio in the polar stratosphere and low mesosphere from a multi-year set of MIPAS-ENVISAT limb-scanning measurements
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Monthly mean vertical profiles of pressure, temperature and water vapour volume mixing ratio in the polar stratosphere and low mesosphere from a multi-year set of MIPAS-ENVISAT limb-scanning measurements

机译:来自多年MIPAS-ENVISAT肢体扫描测量结果的极平流层和中低层中压力,温度和水蒸气体积混合比的月平均垂直分布图

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Measurements performed at polar latitudes by the MIPAS limb-scanning Fourier Transform spectrometer aboard ENVISAT, from July 2002 to March 2004 (FR mission) and January 2005 to April 2010 (OR mission) were analysed with the 2-D tomographic Geofit Multi-Target Retrieval (GMTR) procedure (Dinelli et al., 2010. The MIPAS2D database of MIPAS/ENVISAT measurements retrieved with a multi-target 2-dimensional tomographic approachAtmos. Meas. Techn. Discuss. (AMTD) 2, 2639-2688.) to obtain the MIPAS2D database, and extract more than 386,000 vertical profiles of pressure p, temperature T and water vapour volume mixing ratio Q. They were subdivided into 12 latitudinal classes selected in steps of 5° from 65°N to 90°N and 65°S to 90°S, each vertical profile consisting of values measured at 14 altitude levels from 12 to 60. km. Each latitudinal set was subdivided into 12 monthly sets to determine the multi-year monthly mean vertical profiles of the three parameters: those of p (monthly average standard deviations (SD) 5-15%) provide evidence of marked seasonal variations above 30. km; those of T (SD values of a few percent) show large seasonal variations, with summer maxima at all stratospheric levels; and those of Q (SD lower than 20% from 20 to 50. km) present values ranging in general between 2 and 6. ppmv at the 12-25. km levels and 4 and 7. ppmv at higher altitudes. To verify the reliability of the MIPAS results, the pressure profiles are compared with those obtained from radiosounding data-sets taken at Arctic and Antarctic sites from 2000 to 2003; those of T with both radiosounding measurements and MLS/Aura satellite data from 2005 to 2010; and those of Q with the MLS/Aura satellite data, finding a substantial agreement in all cases. Comparison of MIPAS pressure and temperature profiles with pre ozone-hole CIRA models at 70° and 80° latitudes highlights the variations occurring in the polar atmosphere over the last 3 decades, with relative pressure decreases of 5-10% on average, and overall average decreases in temperature of 0.4 and 2.0. K in the Arctic and Antarctica, respectively. Using the MIPAS profiles of p, T and Q, the monthly mean vertical profiles of absolute humidity were also calculated, from which the monthly values of stratospheric water vapour content from 12 to 50. km were determined, varying between 0.0047 and 0.0070. mm at Arctic latitudes and between 0.0026 and 0.0055. mm at Antarctic latitudes.
机译:使用2-D断层摄影Geofit多目标检索分析了ENVISAT上MIPAS肢体扫描傅里叶变换光谱仪在2002年7月至2004年3月(FR任务)和2005年1月至2010年4月(OR任务)在极纬度进行的测量。 (GMTR)程序(Dinelli等,2010。使用多目标二维层析成像方法Atmos。Meas。Techn。Discuss(AMTD)2,2639-2688检索的MIPAS / ENVISAT测量的MIPAS2D数据库)。 MIPAS2D数据库,并提取了超过386,000的压力p,温度T和水蒸气体积混合比Q的垂直分布图。将它们细分为12个纬度类别,从65°N到90°N和65°S以5°为步长至90°S,每个垂直剖面都包含在12至60. km的14个海拔高度测量的值。每个纬度集细分为12个月集,以确定三个参数的多年月平均垂直分布:p的分布(月平均标准差(SD)5-15%)提供了超过30. km的明显季节性变化的证据。 ; T值(标准偏差的百分之几)显示出较大的季节变化,所有平流层均具有夏季最大值; Q值(从20到50. km,SD低于20%)的值通常在12至25之间为ppmv。公里级别和4和7. ppmv在更高的高度。为了验证MIPAS结果的可靠性,将压力剖面与从2000年至2003年在北极和南极地点获取的无线电探测数据集获得的压力剖面进行了比较。 T在2005年至2010年期间的声音测量结果和MLS / Aura卫星数据;以及Q的MLS / Aura卫星数据,发现在所有情况下都具有实质性的一致性。将MIPAS压力和温度曲线与70°和80°纬度上的臭氧前孔CIRA模型进行比较,可以发现过去30年中极地大气中的变化,相对压力平均降低了5-10%,整体平均温度降低0.4和2.0。分别在北极和南极洲的K。使用p,T和Q的MIPAS分布图,还可以计算出绝对湿度的月平均垂直分布图,从中可以确定平流层水蒸气含量在12至50. km之间的月度值,介于0.0047和0.0070之间。北极纬度为0.0026至0.0055之间的毫米。在南极纬度处为mm。

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