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Formaldehyde and nitrogen dioxide over the remote western Pacific Ocean: SCIAMACHY and GOME-2 validation using ship-based MAX-DOAS observations

机译:遥远的西太平洋上空的甲醛和二氧化氮:SCIAMACHY和GOME-2验证,使用舰载MAX-DOAS观测

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In October 2009, shipborne Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) measurements were performed during the TransBrom campaign over the western Pacific Ocean (≈ 40° N to 20° S). Vertical tropospheric trace gas columns and profiles of nitrogen dioxide (NO_2) and formaldehyde (HCHO) as well as stratospheric NO_2 columns were retrieved in order to validate corresponding measurements from the GOME-2 and SCIAMACHY satellite instruments and to estimate tropospheric background concentrations of these trace gases. All instruments reproduced the same characteristic, latitude-dependent shape of stratospheric NO_2. SCIAMACHY and GOME-2 data differ by about 1% from each other while yielding lower vertical columns than MAX-DOAS morning values as a consequence of measurement time and stratospheric NO_2 diurnal cycle. Due to this diurnal cycle, an increase of 8.7 ± 0.5 × 10~(13) molec cmg~(-2) h~(-1) of stratospheric NO_2 was estimated from MAX-DOAS data at low latitudes during the day. Tropospheric NO_2 was above the detection limit only in regions of higher anthropogenic impact (ship traffic, transport of pollution from land). A background column of 1.3 × 1014 molec cm~(-2) (or roughly 50 ppt boundary layer concentration) can be estimated as upper limit for the remote ocean, which is in agreement with GOME-2 monthly mean values. In the marine boundary layer close to the islands of Hokkaido and Honshu, up to 0.8 ppbv were retrieved close to the surface. Background HCHO concentrations over the remote ocean exhibit a diurnal cycle with maximum values (depending strongly on weather conditions) of 4 × 10~(15) molec cm~(-2) for the vertical column at noontime. Corresponding peak concentrations of up to 1.1 ppbv were retrieved in elevated altitudes (≈ 400 m) around noon while maximum concentrations in the evening are close to the ground. An agreement between MAX-DOAS and GOME-2 data was found for typical vertical columns of 3 × 10~(15) molec cm~(-2) over the remote ocean at the time of overpass.
机译:2009年10月,在西太平洋(≈40°N至20°S)的TransBrom运动期间,进行了船载多轴差分光学吸收光谱(MAX-DOAS)测量。检索了垂直对流层微量气柱和二氧化氮(NO_2)和甲醛(HCHO)以及平流层NO_2柱的分布图,以验证来自GOME-2和SCIAMACHY卫星仪器的相应测量并估算这些迹线的对流层本底浓度气体。所有仪器都再现了平流层NO_2的相同特征,取决于纬度的形状。 SCIAMACHY和GOME-2数据彼此相差约1%,但由于测量时间和平流层NO_2昼夜周期的缘故,垂直柱比MAX-DOAS早晨值低。由于这一昼夜周期,根据白天低纬度地区的MAX-DOAS数据,估计平流层NO_2的增加量为8.7±0.5×10〜(13)摩尔cmg〜(-2)h〜(-1)。对流层NO_2仅在人为影响较大的地区(船舶交通,陆地污染运输)高于检测极限。可以估算出1.3×1014摩尔cm〜(-2)的背景柱(或大约50 ppt边界层浓度)作为偏远海洋的上限,这与GOME-2的月平均值一致。在北海道和本州岛附近的海洋边界层中,在表层附近的储水量高达0.8 ppbv。在中午,垂直海洋柱上的本底HCHO浓度表现出一个昼夜周期,最大值(强烈取决于天气条件)为4×10〜(15)mol·cm〜(-2)。在中午前后升高的海拔(≈400 m)中检索到了高达1.1 ppbv的相应峰值浓度,而晚上的最大浓度接近地面。立交时,偏远海洋上典型的3×10〜(15)摩尔cm〜(-2)的典型垂直柱的MAX-DOAS与GOME-2数据之间存在一致性。

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