Correction to “Modelling the Black Carbon Variability and Dynamics in Almaty, Kazakhstan, During Winter and Summer Seasons”

IF 3.1 4区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES
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引用次数: 0

Abstract

Tursumbayeva, M., G. Ciarelli, L. Di Antonio, M. Bettineschi, D. Kissebayev, and N. Baimatova. 2026. “ Modelling the Black Carbon Variability and Dynamics in Almaty, Kazakhstan, During Winter and Summer Seasons.” Meteorological Applications 33, no. 3: e70183. https://doi.org/10.1002/met.70183.

In the originally published article, the sequence of Figures 2-4 was incorrect. The corrected version is shown below.

Additionally, the in-text citations for Figures 3 and 4 were corrected in the following sentences:

Fifth paragraph, third sentence in 3.2.1 | Meteorological Conditions

At night (from 22 to 08), it reproduced the prevailing southerly winds, while during the daytime (11–19) the direction reversed to northerly winds (Figures 2 and 3).

Second paragraph in 3.2.2 | Vertical Profiles

Since comparison of PBLH derived from the model and observations was difficult (Figures S14 and S15) due to the coarser resolution of the radiosonde profiles in winter, it was decided to compare the observed potential temperature values directly with the model to minimize uncertainties (Figure 4).

Third paragraph, first sentence in 3.2.2 | Vertical Profiles

Figure 4 shows the diurnal and seasonal patterns in potential temperature in January and July 2023.

Fourth paragraph, first sentence in 3.2.2 | Vertical Profiles

In January, the profiles at 06 LT show a stratified atmosphere and the presence of a temperature inversion, while at 18 LT the temperature inversion is weaker (Figure 4).

The online version of this article has been corrected accordingly.

We apologize for these errors.

Abstract Image

对“哈萨克斯坦阿拉木图冬季和夏季黑碳变率和动态模拟”的修正
M. Tursumbayeva, G. Ciarelli, L. Di Antonio, M. Bettineschi, D. Kissebayev和N. Baimatova. 2026。“对哈萨克斯坦阿拉木图冬季和夏季黑碳变化和动态的建模”。气象应用33,第33期。3: e70183。https://doi.org/10.1002/met.70183。在最初发表的文章中,图2-4的顺序是错误的。更正后的版本如下所示。另外,对图3和图4的文内引用作以下更正:3.2.1 |气象条件第5段第3句在夜间(22 - 08)再现了盛行的南风,而在白天(11-19)则逆转为北风(图2和图3)。由于冬季探空廓线的分辨率较粗,模型得到的PBLH与观测数据比较困难(图S14和S15),因此决定直接将观测到的潜在温度值与模型进行比较,以尽量减少不确定性(图4)。图4为2023年1月和7月潜在温度的日变化和季节变化。1月份,06 LT的垂直剖面显示出分层大气和逆温的存在,而18 LT的逆温较弱(图4)。本文的在线版本已进行了相应的更正。我们为这些错误道歉。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Meteorological Applications
Meteorological Applications 地学-气象与大气科学
CiteScore
5.70
自引率
3.70%
发文量
62
审稿时长
>12 weeks
期刊介绍: The aim of Meteorological Applications is to serve the needs of applied meteorologists, forecasters and users of meteorological services by publishing papers on all aspects of meteorological science, including: applications of meteorological, climatological, analytical and forecasting data, and their socio-economic benefits; forecasting, warning and service delivery techniques and methods; weather hazards, their analysis and prediction; performance, verification and value of numerical models and forecasting services; practical applications of ocean and climate models; education and training.
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