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南京气溶胶光学特性地基观测研究

王静 牛生杰 许丹

气象科学2017,Vol.37Issue(2):248-255,8.
气象科学2017,Vol.37Issue(2):248-255,8.DOI:10.3969/2016jms.0049

南京气溶胶光学特性地基观测研究

Ground-based observation of aerosol optical properties in Nanjing

王静 1牛生杰 1许丹1

作者信息

  • 1. 南京信息工程大学 中国气象局气溶胶与云降水重点开放实验室,南京210044
  • 折叠

摘要

Abstract

By using the ground-based observation retrieval data from CE318 sun-photometer in Nanjing of 2003,the variation characteristics of aerosol optical properties were analyzed.Moreover,the graphical method was used to analyze the aerosol type classification.Results show that the maximum of the Aerosol Optical Depth (AOD) in Nanjing occurred in January (0.97±0.49),the minimum one appeared in July (0.53±0.37),and the annual mean value was 0.71±0.42;except March,the value of (A)ngstr(o)m exponent α was 0.8 higher in the rest months,and the maximum value appeared in August and December(1.24±0.17);the seasonal mean value of AOD in winter (0.85±0.47) and spring (0.72±0.45) were slightly higher than that in summer (0.63±0.40) and autumn (0.62±0.36),and the seasonal mean value of α were as follows:winter (1.18±0.16) >summer(1.15±0.32) >autumn (1.05±0.33)>spring (0.86±0.21).The diurnal variation of AOD presented high value in the morning and evening and relatively stable during the day,however,a single peak existed in winter,which appeared at 13:00 with the value of 1.05±0.64.Industrial and urban composite pollution caused by fine particle pollution accounted for a relatively high proportion.The most frequent distribution of AOD and α with the peak center at 0.53 and 1.2 accounted for 21% and 16%.The AOD high value area(>0.7) in Nanjing data mainly centered in the fine mode growth part(1.0<α< 1.4,δα<0,η~70%),and aerosol fine mode size ranged from 0.10 to 0.15 μm.

关键词

气溶胶光学特性/气溶胶光学厚度/太阳光度计/南京

Key words

Aerosol optical properties/AOD/Sunphotometer/Nanjing

分类

天文与地球科学

引用本文复制引用

王静,牛生杰,许丹..南京气溶胶光学特性地基观测研究[J].气象科学,2017,37(2):248-255,8.

基金项目

国家自然科学基金资助项目(41375138,41275151,41305034) (41375138,41275151,41305034)

江苏省基础研究计划(自然科学基金)青年基金项目(BK20130993) (自然科学基金)

气象科学

OA北大核心CSTPCD

1009-0827

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