The Climatic from Troposphere to Lower Stratosphere at Mid-latitude Along 120° E and Its Relation with Ozone Variation

Ge Ling    Zhao Yuandong

Vol.10, NO.4, 1999

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Article Navigation > Journal of Applied Meteorological Science > 1999 > 10(4): 445-452

Ge Ling, Zhao Yuandong. The climatic from troposphere to lower stratosphere at mid-latitude along 120°E and its relation with ozone variation. J Appl Meteor Sci, 1999, 10(4): 445-452.

Citation:

Ge Ling, Zhao Yuandong. The climatic from troposphere to lower stratosphere at mid-latitude along 120°E and its relation with ozone variation. J Appl Meteor Sci, 1999, 10(4): 445-452.

Ge Ling, Zhao Yuandong. The climatic from troposphere to lower stratosphere at mid-latitude along 120°E and its relation with ozone variation. J Appl Meteor Sci, 1999, 10(4): 445-452.

Citation:

Ge Ling, Zhao Yuandong. The climatic from troposphere to lower stratosphere at mid-latitude along 120°E and its relation with ozone variation. J Appl Meteor Sci, 1999, 10(4): 445-452.

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The Climatic from Troposphere to Lower Stratosphere at Mid-latitude Along 120° E and Its Relation with Ozone Variation

Ge Ling Zhao Yuandong,

1.
1) (Nanjing Institute of Meteorology, Nanjing 210044); 2) (National meteorological center, Beijing 100081)

Publish Date: 1999-11-30

Abstract

Abstract

Using the mean monthly temperature data of Nanjing, Shenyang and Hailar from surface to 30 hPa during 1958 to 1995, the variable features on the climatic variability of the regions along 120° E from 30° N to 50° N with altitude-latitude-season are studied, and the relations with ozone variation in East Asia, adjacent area of same latitude and Eurasia key areas of high-latitude are also discussed.
- Troposphere;
- Lower stratosphere;
- Climatic variation