Defining the Feature of Cold Wave (Al-Marba'aniyah) in Iraq Defining the Feature of Cold Wave (Al-Marba'aniyah) in Iraq

Abstract

Abstract:
Al-Marba'aniyah, which is a long cold wave, was defined by ancient
Iraqis. It represents the coldest days in Iraq. In this research paper, a new
scale was put to define it. It shows that the period between the minimum
temperature degree recoded in December and the minimum temperature
degree recorded in January is considered to be the period of Al-Marba'aniyah.
The research concluded that Al-Marba'aniyah is unsteady and it changes in
the days of its occurrence. It was also concluded that the dates of the
beginning and the end of Al-Marba'aniyah are unsteady, too. Moreover, it was
found out that each of the Siberian high, European high, and finally the
subtropical high are the responsible systems for the beginning and the end of
Al-Marba'aniyah. In addition to this, it was concluded that during the evolution
of Al-Marba'aniyah, the tropical ridge (Geopotential high 500 mb)
enormously associates with the surface high pressure and that, during the
decay of Al- Al-Marba'aniyah, the cold troughs enormously associates with the
surface high pressure.