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News Update on Troposphere Research: Oct – 2019

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Stratosphere‐troposphere exchange

In the past, studies of stratosphere‐troposphere exchange of mass and chemical species have primarily stressed the synoptic‐ and small‐scale mechanisms of exchange. This review, however, includes conjointly the global‐scale aspects of exchange, like the transport across associate degree physical property surface (potential temperature regarding 380 K) that within the tropics lies simply on top of the layer, close to the 100‐hPa physical phenomenon. Such a surface divides the layer into associate degree “overworld” associate degreed an extratropical “lowermost stratosphere” that for transport functions have to be compelled to be sharply distinguished. This approach places stratosphere‐troposphere exchange within the framework of the final circulation and helps to clarify the roles of the various mechanisms concerned and therefore the interaction between giant and tiny scales. The role of waves and eddies within the extratropical overworld is stressed. [1]

A Stratosphere-Troposphere Data Assimilation System

A data assimilation system has been developed at the united kingdom meteorologic workplace to investigate the combo of observations accessible within the layer and layer. the info assimilation system is predicated on the analysis correction theme used at the united kingdom meteorologic workplace for operational prediction.

The assimilation system is presently being employed to produce close to time period analyses of meteorologic fields from the layer and layer to the higher Atmosphere analysis Satellite (UARS) Science Team. At this stage, these analyses are supported the same set of observations to the operational analyses, so that they offer associate freelance check of the UARS observations. within the layer they’re mostly supported soundings from the National Oceanic and part Administration polar orbiters. [2]

The changing photochemistry of the troposphere

The chemistry of the layer is well influenced by a large vary of chemical processes that square measure primarily driven by the action of star ultraviolet light of wavelengths shorter than regarding 310 nm on gas and vapour. This results in the formation of hydroxyl group (OH) radicals that, despite terribly low tropospheric concentrations, take away most gases that square measure emitted into the atmosphere by natural and anthropogenetic processes. though tropospheric gas solely makes up regarding 100% of all atmospherical gas, through the formation of OH, it determines the oxidization potency of the atmosphere and it’s, therefore, of the utmost importance for maintaining the chemical composition of the atmosphere. [3]

Important evidence of constant low CO2 windows and impacts on the non-closure of the greenhouse effect

The CO2 distribution in the atmosphere remains unclear for the complexity of the long-range vertical transport process and other influencing factors. In this work, regression analysis was used to verify the accuracy of CO2 concentrations datasets. Geostatistical analyses were used to investigate the spatiotemporal distributions of CO2 at 7 levels from near the surface to the mid-troposphere (0~5 km). Spatial correlation and time series analyses were used to further determine the diffusion characteristics of the CO2 concentration based on the horizontal wind (NCEP R2), which is one of the main driving factors. [4]

Atmospheric Stability across the Lower Troposphere in Enugu City, Nigeria

This study surveyed the atmospherical stability pattern within the lower layer over Enugu from 2010-2015. The wide and tolerably used Pasquill-Gifford stability theme was used in evaluating the steadiness classes. Six-hourly synoptic information parameters for temperature, wind speed and inclementness nonheritable from the Era-Interim platform at one thousand mbar pressure were utilized in the analysis. the information were obtained at zero.125 degree resolution. Results showed that terribly stable stability categories D (neutral), E (stable), and F (very stable) conditions occurred throughout the night and early hours of dawn. Also, whereas category D dominated throughout the wet season, categories E and F delineated  a reverse trend throughout the time of year. [5]


[1] Holton, J.R., Haynes, P.H., McIntyre, M.E., Douglass, A.R., Rood, R.B. and Pfister, L., 1995. Stratosphere‐troposphere exchange. Reviews of geophysics, 33(4), (Web Link)

[2] Swinbank, R. and O’Neill, A., 1994. A stratosphere-troposphere data assimilation system. Monthly Weather Review, 122(4), (Web Link)

[3] Crutzen, P.J. and Zimmermann, P.H., 1991. The changing photochemistry of the troposphere. Tellus A: Dynamic Meteorology and Oceanography, 43(4), (Web Link)

[4] Important evidence of constant low CO2 windows and impacts on the non-closure of the greenhouse effect
Jing Zhao, Guoqing Li, Weihong Cui, Qianqian Cao & Haoping Zhang
Scientific Reports volume 9, Article number: 5033 (2019) (Web Link)

[5] O. Edokpa, D. and O. Nwagbara, M. (2018) “Atmospheric Stability across the Lower Troposphere in Enugu City, Nigeria”, Journal of Geography, Environment and Earth Science International, 15(2), (Web Link)

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