尼泊尔两个城市的碳质气溶胶和太阳总辐射情景

R. Sharma, B. Bhattarai, B. Sapkota, Mohan B. Gewali, B. Kjeldstad
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摘要

在加德满都和比拉特纳加尔使用ae - 31,7通道浓度计测量了元素碳(EC)和黑碳(BC)气溶胶;2011年1月至5月,对尼泊尔两个特大城市进行了为期5个月的研究,研究其时空变化。利用Kipp和Zonen cmp6辐射计监测太阳总辐射。在两个研究地点,EC和BC的月浓度变化是明显的。在比拉特纳格尔,月EC浓度在3.3 -20.7 µg / m3之间变化,而在加德满都,月EC浓度在6.0-13.7 µg / m3之间变化。同样,BC的月浓度范围分别为3.3 -20.1 µg / m3和7.0-14.9 µg / m3。结果表明,1月份两个站点的EC和BC均为最高,并逐渐降低。月平均太阳辐射在5月最大,1月最小。观测到月平均碳质气溶胶与太阳总辐射之间存在明显的反相关。此外,碳质气溶胶EC和BC的日变化都很明显,在当地时间上午9点左右和晚上20点左右出现两个高峰,下午浓度最低。两个地点峰的性质不同。比拉特纳格尔的傍晚高峰更大,而加德满都的早晨高峰更大,这可以推断出傍晚和早晨分别有大量的家庭和工业燃料消耗活动。除此之外,在Biratnagar, EC的日和月浓度高于BC,反映了家庭、工业和其他城市活动的生物质燃料消耗略高于化石燃料。与此相反,加德满都显示化石燃料比生物燃料更占主导地位,因为碳质气溶胶的浓度相反。太阳总辐射在两个地点也有明显的日变化,在正午左右达到最大值。
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The Scenario of Carbonaceous Aerosols and Total Solar Radiation in Two Cities in Nepal
Measurement of elemental carbon (EC) and black carbon (BC) aerosols was carried out using AE-31, 7 channel aethalometer at Kathmandu and Biratnagar; two mega cities of Nepal, for five months, January to May 2011 to study its temporal and spatial variation. Total solar radiation was also monitored using Kipp and Zonen CMP 6 pyranometer. Monthly concentration variation for EC and BC was distinct in both study sites. At Biratnagar, monthly EC concentration varies from 3.3 -20.7 µg /m 3 while in Kathmandu it varies between 6.0-13.7 µg /m 3 . Similarly, BC monthly concentration ranges from 3.3 -20.1 µg /m 3 and 7.0-14.9 µg /m 3 respectively. It was found that both EC and BC were highest during January in both the sites and it decreases gradually. Monthly average solar radiation shows a maximum value in May and minimum in January. A distinct anti-correlation between monthly average carbonaceous aerosols and total solar radiation was observed. Moreover, there was a pronounced diurnal variation of both carbonaceous aerosols EC and BC in the sites with two high peaks one in the morning at about 9:00 and another at late evening 20:00 local time with minimum concentration in the afternoon. The nature of peaks were different at two sites. Biratnagar shows a larger evening peak while Kathmandu shows in the morning inferring heavy domestic and industrial fuel consuming activities in evening and morning respectively. In addition to this, daily and monthly concentration of EC was more than BC at Biratnagar reflecting slightly more biomass fuel consumption than fossil fuel for domestic, industrial and other urban activities. In contrast to this, Kathmandu shows more domination of fossil fuel than biofuel because of reverse order concentration of carbonaceous aerosols. Total solar radiation also shows apparent diurnal variation in both sites with the highest value at around noon time.
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