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Mean global and regional distributions of MOPITT carbon monoxide during 2000-2009 and during ENSO

机译:MOPITT一氧化碳在2000-2009年和ENSO期间的全球和区域平均分布

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摘要

The MOPITT (Measurements Of Pollution In The Troposphere) CO measurements over a 10-year period (2000-2009) reveal consistently positive trends on the order of 0.13-0.19 × 10~(16) mol cm~(-2) per month in CO total column concentrations over the entire globe and the hemispheres. Two maxima in globally averaged CO concentrations are identified: one in April and one in October, with two minima in July and December. These maxima and minima are attributable to the respective maxima and minima in CO concentrations over the Northern and Southern Hemispheres. Over the Tropics, maximum and minimum CO concentrations are noted in October and June, respectively, due primarily to biomass burning. During El Niflo DJF (December-January-February) and JJA (June-July-August), predominantly positive anomalies in CO total column are noted over the entire globe except for the high latitudes of both hemispheres and the central part of the South America where negative anomalies are identified. La Nifia DJF and JJA are largely opposite to El Niflo DJF and JJA in CO total column anomalies. Negative (positive) anomalies in CO total column tend to be associated with wet (dry) anomalies in precipitation over the major polluted areas during ENSO. It is suggested that changes in the atmospheric circulations during ENSO either enhance or weaken precipitation systems with the associated precipitation modulating CO total column. The correspondence between anomalies in CO total column and anomalies in Terra MODIS fire pixels during ENSO is rather poor over many parts of the world.
机译:MOPITT(对流层污染测量)在10年期间(2000-2009年)的CO测量显示,在2004年,每月的持续积极趋势约为0.13-0.19×10〜(16)mol cm〜(-2)。整个地球和整个半球的CO总柱浓度。确定了全球平均CO浓度的两个最大值:一个在4月和一个在10月,两个在7月和12月达到最小值。这些最大值和最小值可归因于北半球和南半球的CO浓度各自的最大值和最小值。在热带地区,主要由于生物质燃烧,分别在10月和6月记录了最高和最低CO浓度。在El Niflo DJF(12月至1月至2月)和JJA(6月至7月至8月)期间,除了整个半球和南美洲中部的高纬度地区外,整个全球的CO总量列主要呈正异常。识别出负异常的地方。 La Nifia DJF和JJA在CO总色谱柱异常方面与El Niflo DJF和JJA相反。在ENSO期间,CO总柱中的负(正)异常往往与主要污染区降水的湿(干)异常有关。建议在ENSO期间大气环流的变化会通过相关的降水调节CO总塔来增强或减弱降水系统。在世界许多地方,在ENSO期间,CO总计列中的异常与Terra MODIS火像素中的异常之间的对应性很差。

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  • 来源
    《Atmospheric environment》 |2011年第6期|p.1347-1358|共12页
  • 作者

    Yongxin Zhang;

  • 作者单位

    Research Applications Laboratory, National Center for Atmospheric Research, 3450 Mitchell Lane, Boulder, CO, USA;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    MOPITT CO; ENSO; fire;

    机译:MOPITT CO;ENSO;四;

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