شناسایی تغییرات ارتفاع ژئوپتانسیل، تاوایی و فشار تراز دریای الگوهای گردش جوی غالب مؤثر بر اقلیم ایران‎زمین

Introduction
The changes in behaviour of climate and meteorological parameters are closely related to
changes in atmospheric circulation. The analysis of historical atmospheric troposphere
circulation is critically important to global and regional climate change and extremes with
regard to its dynamical features. The circulation changes are manifested by a gradual reduction
in high-latitude sea-level pressure, and an increase in mid-latitude sea-level pressure associated
with one phase of the Arctic Oscillation (a hemisphere-scale version of the North Atlantic
Oscillation. Recent observations have found that the tropical belt running around the equator has
grown wider, and has expanded by around 2° to 5° latitude and into the adjacent subtropical
regions since 1979. Global greenhouse gas emissions contribute to expansion of the tropics
(about 0.05° per decade)in the northern hemisphere tropics. The effect of black carbon and
troposphere ozone emissions are about twice the size of those due to greenhouse gases alone
(about 0.07° to 0.12° per decade). The aim of this study is investigation of variability in the
intensity of the monthly geo-potential height, vorticity and sea level pressure over synoptic
circulation patterns impacting Iran.
Methodology
In order to accomplish this research, daily grid data with spatial resolution of 2.5􀵈2.5 degree
during 1/1/1960 to 31/12/2012 have been extracted from NCEP/NCAR database. The monthly
average sea level pressure and geo-potential height in level of 1000 hectopascal is calculated to

detect the action of spatial kernel of each synoptic system. The for this investigation is including
daily zonal and meridian wind components (Uwnd and Vwnd) data, geopotential height data for
each levels of 1000, 850, 700 and 500 hectopascal levels, and sea level pressure. Vorticity is
calculated by Uwnd and Vwnd components. Then monthly mean is also calculated for each
levels separately. Although some circulation patterns can operate in special months and seasons
of year but trend analysis has been evaluated for each circulation patterns in whole months and
seasons. To detect time series trend, nonparametric Mann Kendal statistic test has been applied.
The trend has been tested in 95% confidence level. Sen Estimator is used to calculate trend
slope rate.
Results and Discussion
Siberian anticyclone, Sudan cyclone, Mediterranean region cyclones (East Mediterranean,
Mediterranean and Black sea) and Monsoon and Persian Gulf cyclones have been selected
according to the maps of sea level pressure and geopotential monthly means. In total vorticity,
geopotential height in different levels and sea level pressure have significant trend in 95%
confidence level. The highest variation is observed for high levels at 700 and 500 hectopascal.
In winter season, sea level pressure, vorticity and geopotential in 1000, 850, 700 and 500
hectopascal levels don’t show significant trend. While in spring and summer the trend of
vorticity in four selected levels is significant and negative, geopotential height and sea level
pressure have positive significant trend. Over cyclonic systems in Mediterranean region, the sea
level pressure and geopotential height show increasing trend especially in winter season. The
slope positive trend on the Sudan is significant in winter. The trend of geopotential height in
four selected levels in winter is positive and significant. In other seasons, the trend is positive
except in 1000 hectopascal level. Over Monsoon cyclone system in all seasons, geopotential
height is increasing from 1000 to 500 hectopascal levels. Vorticity trend in low levels at 1000
and 850 hectopascal is positive. The increasing geopotential height over Persian Gulf is smaller
than other atmospheric circulation patterns especially in low levels. Vorticity rate contrary to
other systems is increasing.
Conclusion
Increasing sea level pressure and geopotential height over cyclonic circulation patterns of Sudan
and Mediterranean regions especially in cold seasons of year (winter and autumn) result in a
decrease in systems cyclonic action, sea level gradient pressure, instability and precipitation in
region. In warm seasons of year (spring and summer) negative trend of vorticity and positive
trend of sea level pressure and geopotential height result in decrease in warm seasons
precipitation and increase in stability. The results of this study agree with findings of some other
researchers about increase in warming of troposphere, changes in synoptic systems intensity,
instability increase and negative vorticity increase in north hemisphere.