Temperature altitude amplification as a footprint of a possible anthropogenic impact on the climate of Australia
Autor: | Dragan Buric, Jovan Mihajlovic, Vladan Ducic, Ljubomir Popovic |
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Rok vydání: | 2015 |
Předmět: |
Geography (General)
Geography Planning and Development Australia Australia temperature trend temperature altitude amplification TLT TMT lcsh:G1-922 temperature Geology Atmospheric sciences Footprint (electronics) trend Altitude Tourism Leisure and Hospitality Management TMT TLT G1-922 temperature altitude amplification Environmental science lcsh:Geography (General) Earth-Surface Processes Demography |
Zdroj: | Zbornik radova Geografskog instituta "Jovan Cvijić", SANU Zbornik Radova: Geografski institut "Jovan Cvijić", Vol 65, Iss 3, Pp 297-307 (2015) Zbornik Radova: Geografski institut "Jovan Cvijić", Vol 65, Iss 3 (2015) |
ISSN: | 1821-2808 0350-7599 |
DOI: | 10.2298/ijgi1503297b |
Popis: | In the conditions of dominant influence of anthropogenic greenhouse effect and according to simulation models, a more intensive temperature increase in upper-air layers of troposphere than in lower-air layers should be expected. In order to check this, the difference between temperature trends in the middle and lower troposphere over the Australian continent has been analyzed. Satellite data UAHMSU for lower troposphere (TLT) and middle troposphere (ТМТ), for the 1979-2014 period have been used in the study. Estimates have been done on seasonal and annual value, and the results obtained indicate that there is a trend of temperature increase, but not altitude amplification over Australia. Reducing the time series for a year from the beginning (1980-2014, 1981-2014…), a comparative analysis between corresponding time series for each season, i.e., each year, showed that from 140 mutual comparisons, altitude amplification does not exist in 130, i.e., in 93% of cases. Moreover, in sub-periods of 1996 (1997-2014, 1998- 2014…), we can not even talk about warming in most cases because the trend of temperature is negative. |
Databáze: | OpenAIRE |
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