VARIATIONS OF AIR TEMPERATURE AT 850 HPA IN NORTH-WEST ROMANIA

The 850 hPa air pressure level is situated about 1.5 km above sea level. This means that the surface does not influence the temperature at this altitude, so the diurnal temperature variations are small. They are about 2-3 degrees, or they do not exist, at all. This is why temperature of the 850 hPa...

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Main Author: MAIER N.
Format: Article
Language:English
Published: Cluj University Press 2015-03-01
Series:Aerul şi Apa: Componente ale Mediului
Subjects:
Online Access:http://aerapa.conference.ubbcluj.ro/2015/PDF/25_MAIER_187_192.pdf
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author MAIER N.
author_facet MAIER N.
author_sort MAIER N.
collection DOAJ
description The 850 hPa air pressure level is situated about 1.5 km above sea level. This means that the surface does not influence the temperature at this altitude, so the diurnal temperature variations are small. They are about 2-3 degrees, or they do not exist, at all. This is why temperature of the 850 hPa level is used for identification of air masses and location of warm and cold fronts. Moreover, temperature variation of the 850 hPa level can be analysed in themselves, as indicators of climate 1500 meters above the sea level. The 1973-2014 period, analysed in this study, was chosen as the longest available series in Cluj-Napoca. The results, concerning the evolution of temperature at this standard isobaric level pointed at strong warming in the last 10-15 years. In the last 7 years the highest temperatures were higher by one degree at the 850 hPa lever than in the preceding years. The heating at the analyzed isobaric level overlaps the growing of ground temperature, analyzed the medium annual temperature in the period 1973-2014.
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spelling doaj.art-d57e92ed5d8a425596a3bdeb2f79d4972023-12-02T00:21:51ZengCluj University PressAerul şi Apa: Componente ale Mediului2067-743X2015-03-01201518719210.17378/AWC2015_25VARIATIONS OF AIR TEMPERATURE AT 850 HPA IN NORTH-WEST ROMANIAMAIER N.0Regional Meteorological Center Transilvania Nord, Cluj - Napoca, Romania The 850 hPa air pressure level is situated about 1.5 km above sea level. This means that the surface does not influence the temperature at this altitude, so the diurnal temperature variations are small. They are about 2-3 degrees, or they do not exist, at all. This is why temperature of the 850 hPa level is used for identification of air masses and location of warm and cold fronts. Moreover, temperature variation of the 850 hPa level can be analysed in themselves, as indicators of climate 1500 meters above the sea level. The 1973-2014 period, analysed in this study, was chosen as the longest available series in Cluj-Napoca. The results, concerning the evolution of temperature at this standard isobaric level pointed at strong warming in the last 10-15 years. In the last 7 years the highest temperatures were higher by one degree at the 850 hPa lever than in the preceding years. The heating at the analyzed isobaric level overlaps the growing of ground temperature, analyzed the medium annual temperature in the period 1973-2014.http://aerapa.conference.ubbcluj.ro/2015/PDF/25_MAIER_187_192.pdftemperature850 hPaclimate change
spellingShingle MAIER N.
VARIATIONS OF AIR TEMPERATURE AT 850 HPA IN NORTH-WEST ROMANIA
Aerul şi Apa: Componente ale Mediului
temperature
850 hPa
climate change
title VARIATIONS OF AIR TEMPERATURE AT 850 HPA IN NORTH-WEST ROMANIA
title_full VARIATIONS OF AIR TEMPERATURE AT 850 HPA IN NORTH-WEST ROMANIA
title_fullStr VARIATIONS OF AIR TEMPERATURE AT 850 HPA IN NORTH-WEST ROMANIA
title_full_unstemmed VARIATIONS OF AIR TEMPERATURE AT 850 HPA IN NORTH-WEST ROMANIA
title_short VARIATIONS OF AIR TEMPERATURE AT 850 HPA IN NORTH-WEST ROMANIA
title_sort variations of air temperature at 850 hpa in north west romania
topic temperature
850 hPa
climate change
url http://aerapa.conference.ubbcluj.ro/2015/PDF/25_MAIER_187_192.pdf
work_keys_str_mv AT maiern variationsofairtemperatureat850hpainnorthwestromania