首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Interactive chemistry in the Laboratoire de Meteorologie Dynamique general circulation model: Description and background tropospheric chemistry evaluation - art. no. D04314 [Review]
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Interactive chemistry in the Laboratoire de Meteorologie Dynamique general circulation model: Description and background tropospheric chemistry evaluation - art. no. D04314 [Review]

机译:动力学实验室动态环流模型中的交互化学:描述和背景对流层化学评估-艺术。没有。 D04314 [审阅]

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1] We provide a description and evaluation of LMDz-INCA, which couples the Laboratoire de Meteorologie Dynamique general circulation model (LMDz) and the Interaction with Chemistry and Aerosols (INCA) model. In this first version of the model a CH4 - NOx - CO - O-3 chemical scheme representative of the background chemistry of the troposphere is considered. We derive rapid interhemispheric exchange times of 1.13 - 1.38 years and 0.70 - 0.82 years, based on surface and pressure-weighted mixing ratios of inert tracers, respectively. The general patterns of the nitrogen deposition are correctly reproduced by the model. However, scavenging processes remain a major source of uncertainty in current models, with convective precipitation playing a key role in the global distribution of soluble species. The global and annual mean methane (7.9 years) and methylchloroform (4.6 years) chemical lifetimes suggest that OH is too high by about 19 - 25% in the model. This disagreement with previous estimates is attributed to the missing nonmethane hydrocarbons in this version of the model. The model simulates quite satisfactorily the distribution and seasonal cycle of CO at most stations. At several tropical sites and in the Northern Hemisphere during summer, the OH overestimate leads, however, to a too intense CO chemical destruction. LMDz-INCA reproduces fairly well the distribution of ozone throughout most of the troposphere. A main disagreement appears in the Northern Hemisphere upper troposphere during summer, due to a too high tropopause in the GCM. When the GCM winds are relaxed toward assimilated meteorology, a much higher variability is obtained for ozone in the upper troposphere, reflecting more frequent stratospheric intrusions. The stratospheric influx of ozone increases from 523 Tg/yr in the base case simulation to 783 Tg/yr in the nudged version. [References: 187
机译:1]我们提供了LMDz-INCA的描述和评估,该模型结合了实验室动态气象动力学通用循环模型(LMDz)和化学与气溶胶相互作用(INCA)模型。在该模型的第一个版本中,考虑了代表对流层背景化学的CH4-NOx-CO-O-3化学方案。我们分别基于惰性示踪剂的表面和压力加权混合比得出了1.13-1.38年和0.70-0.82年的快速半球交换时间。该模型正确地再现了氮沉积的一般模式。然而,清除过程仍然是当前模型不确定性的主要来源,对流降水在可溶性物种的全球分布中起着关键作用。全球和年平均甲烷(7.9年)和甲基氯仿(4.6年)的化学寿命表明,该模型中的OH太高了约19-25%。与先前估计的不同之处归因于此版本模型中缺少的非甲烷碳氢化合物。该模型非常令人满意地模拟了大多数站点的CO分布和季节周期。夏季,在几个热带地区和北半球,OH的高估会导致一氧化碳化学破坏太强烈。 LMDz-INCA在整个对流层中都能很好地再现臭氧的分布。由于GCM对流层顶太高,夏季在北半球对流层上部出现了主要分歧。当GCM风向着同化气象方向放宽时,对流层上层的臭氧具有更高的可变性,反映出平流层侵入更加频繁。平流层中的臭氧流入量从基本情况下的523 Tg / yr增加到微动版本的783 Tg / yr。 [参考:187

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