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61.
Urban Atmospheric Chemistry During the PUMA Campaign 2: Radical Budgets for OH,HO<Subscript>2</Subscript> and RO<Subscript>2</Subscript> 总被引:1,自引:0,他引:1
K.?M.?Emmerson N.?CarslawEmail author M.?J.?Pilling 《Journal of Atmospheric Chemistry》2005,52(2):165-183
A detailed photochemical box model was used to investigate the key reaction pathways between OH, HO2 and RO2 radicals during the summer and winter PUMA field campaigns in the urban city-centre of Birmingham in the UK. The model employed
the most recent version of the Master Chemical Mechanism and was constrained to 15-minute average measurements of long-lived
species determined in situ at the site. The results showed that in the summer, OH initiation was dominated by the reactions of ozone with alkenes, nitrous
acid (HONO) photolysis and the reaction of excited oxygen atoms atoms with water. In the winter, ozone+alkene reactions were
the primary initiation route, with a minor contribution from HONO photolysis. Photolysis of aldehydes was the main initiation
route for HO2, in both summer and winter. RO2 initiation was dominated by the photolysis of aldehydes in the summer with a smaller contribution from ozone+alkenes, a situation
that was reversed in the winter. At night, ozone+alkene reactions were the main radical source. Termination, under all conditions,
primarily involved reactions with NO (OH) and NO2 (OH and RCO3). These results demonstrate the importance of ozone+alkene reactions in urban atmospheres, particularly when photolysis reactions
were less important during winter and at nighttime. The implications for urban atmospheric chemistry are discussed. 相似文献
62.
NO<Subscript><Emphasis Type="Italic">x</Emphasis></Subscript> change over China and its influences 总被引:2,自引:0,他引:2
A 3-D chemical transport model (OSLO CTM2) is used to investigate the impact of the increase of NOx emission over China. The model is capable to reproduce basically the seasonal variation of surface NOx and ozone over eastern China. NOx emission data and observations reveal that NOx over eastern China increases quite quickly with the economic development of China. Model results indicate that NOx concentration over eastern China increasingly rises with the increase of NOx emission over China, and accelerates to increase in winter. When the NOx emission increases from 1995 to its double, the ratio of NO2/NOx abruptly drops in winter over northern China. Ozone at the surface decreases in winter with the continual enhancement of the NOx level over eastern China, but increases over southern China in summertime. It is noticeable that peak ozone over northern China increases in summer although mean ozone changes little. In summer, ozone increases in the free troposphere dominantly below 500 hPa.Moreover, the increases of total ozone over eastern China are proportional to the increases of NOx emission.In a word, the model results suggest that the relationship between NOx and ozone at the surface would change with NOx increase. 相似文献
63.
64.
65.
The authors present evidence to suggest that variations in the snow depth over the
Tibetan Plateau (TP) are connected with changes of North Atlantic
Oscillation (NAO) in winter (JFM). During the positive phase of NAO, the
Asian subtropical westerly jet intensifies and the India-Myanmar trough
deepens. Both of these processes enhance ascending motion over the TP. The
intensified upward motion, together with strengthened southerlies upstream
of the India-Myanmar trough, favors stronger snowfall over the TP, which is
associated with East Asian tropospheric cooling in the subsequent late
spring (April--May). Hence, the decadal increase of winter snow depth over
the TP after the late 1970s is proposed to be an indicator of the connection
between the enhanced winter NAO and late spring tropospheric cooling over
East Asia. 相似文献
66.
用1959~1998共40年全球格点风场资料计算了200 hPa与850 hPa的纬向风速差, 即对流层纬向风切变(简称TZWS),并在此基础上得到其距平值。为了全面考察对流层中环流异常的年际变率特征, 根据TZWS的标准差分布, 文中选出了7个TZWS标准差数值大于5 m/s的代表性区域。这7个区域分别位于赤道中太平洋、赤道东太平洋、北太平洋亚热带地区、南太平洋亚热带地区、赤道大西洋、亚洲西南部以及东北部。前5个分别位于赤道、亚热带太平洋和大西洋的区域TZWS指数, 其年际变率与ENSO循环有密切联系, 反映了热带海洋温度异常对低纬度地区对流层环流的影响; 后2个区域的TZWS指数反映的是亚洲西南部和东北部的气候统变率, 在年际时间尺度上与ENSO循环有着明显的区别。通过对全球陆地降水和温度场的分析, 比较了热带、副热带的TZWS指数以及北极涛动指数的异同, 发现后2个区域TZWS指数能很好且能独立反映出北半球中高纬度地区陆地降水及陆地温度的异常模态。 相似文献
67.
采用IGRA提供的2017年81个无线电探空站的探空资料,对4种对流层延迟模型在中国区域的精度进行综合评估与分析。结果表明,GPT2w模型的性能要优于依赖气象参数的Saastamoinen模型及基于球谐函数的GZTD和UNB3m模型;GPT2w模型的偏差均值MB(mean bias)和均方根误差RMSE分别为-0.8 cm和4.1 cm,各测站的MB和RMSE分别处于-2~2 cm和1.3~7.9 cm之间。UNB3m模型在中国区域存在较大的MB和RMSE,模型的RMSE最大可达10.2 cm。4种模型的精度对测站纬度具有一致的敏感性,表现为随测站纬度的升高而降低;模型精度呈明显季节性变化,且不同模型对季节的敏感程度有所差异;对流层湿延迟难以精确建模导致模型精度在夏季(RMSE为6~9 cm)低于冬季(RMSE为2~2.5 cm)。 相似文献
68.
GPS/BDS中长距离RTK定位因为电离层和对流层残余误差的影响,其性能相对于常规RTK有所降低。将GPS/BDS卫星双差电离层误差和对流层误差作为参数,采用卡尔曼滤波进行实时估计。为了验证算法的有效性,利用武汉地区103 km静态基线24 h双频观测数据,分析了GPS和BDS单系统以及二者组合双系统中长距离RTK定位性能。实验结果表明,精确估计的双差电离层残余误差达到米级、对流层误差达到分米级;经过改正后,GPS/BDS单系统的定位精度在1 cm左右,组合双系统则实现了中长距离基线毫米级的高精度定位。 相似文献
69.
ABSTRACTPrevious studies have shown that the recent summer climate (precipitation in particular) over East Asia is varying significantly. Here we extend the study to April, May, and June (AMJ) or the seasonal transition period associated with the onset of the summer monsoon. It is found that the average 1000–400?hPa AMJ tropospheric temperature (TT) experienced a sudden change at the end of the twentieth century. The change has a dipolar modal structure, with one pole over countries in Central Asia (Pakistan, Afghanistan, Uzbekistan, Kazakhstan, Kyrgyzstan, and Tajikistan.) and the other over the Tibetan Plateau. The difference in the TT between the centres of the two poles (?TT), which characterizes the zonal gradient of the TT over Asia, has seen a significant reduction since 1999. The causal relations of ?TT with the local circulation, outgoing longwave radiation (OLR), surface shortwave flux (SSWF), precipitation, etc. have been investigated using a newly developed rigorous causality analysis, which unambiguously reveals a one-way causality from ?TT to each of OLR, SSWF, and precipitation. 相似文献
70.
In order to understand the activity characteristics of low-level jets in the Nanjing area, statistical analysis and comparative study are carried out on their monthly and diurnal variations, characteristics of their cores and accompanying weather conditions using wind profile data in 2005—2008 collected by two wind profilers. The results show that low-level jets have significant monthly and diurnal variations. They occur more frequently in spring and summer than in autumn and winter and are more active in early morning and at night, with the maximum wind speed usually occurring at midnight. The central part of the low-level jet occurs mainly at the height of less than 1400 meters, and the enhancement of central speed is beneficial to the appearance of precipitation. Meanwhile, when the low-level jet appears in summer, it helps cause heavy rain. The statistical results of the boundary wind profiler are well consistent with those of the tropospheric wind profiler. Two kinds of wind profilers also have the capability of continuously detecting the development of low-level jets. 相似文献