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THE HOLY QUR’AN THE LAYERS OF THE EARTH & THE EARTH DISGORGES ITS CHARGES. BASED ON THE WORKS OF HARUN YAHYA WWW.HARUNYAHAY.COM and others PREPARED BY fereidoun.dejahang@ntlworld.com Dr F.Dejahang, BSc CEng, BSc (Hons) Construction Mgmt, MSc, MCIOB, .MCMI, PhD. The Holy
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THE HOLY QUR’AN THE LAYERS OF THE EARTH &THE EARTH DISGORGES ITS CHARGES BASED ON THE WORKS OF HARUN YAHYA WWW.HARUNYAHAY.COMand others PREPARED BY fereidoun.dejahang@ntlworld.com Dr F.Dejahang, BSc CEng, BSc (Hons) Construction Mgmt, MSc, MCIOB, .MCMI, PhD
The Holy Qur'an is the Word of Allah
The height of the tropopause • The height of the tropopause depends on the location, notably the latitude, as shown in the figure on the right (which shows annual mean conditions). It also depends on the season (1, 2). Thus, it is about 16 km high over Australia at year-end, and between 12 - 16 km at midyear, being lower at the higher latitudes. At latitudes above 60�
The height of the tropopause • The tropopause is less than 9 -10 km above sea level; the lowest is less than 8 km high, above Antarctica and above Siberia and northern Canada in winter. • The highest average tropopause is over the oceanic warm pool of the western equatorial Pacific, about 17.5 km high, and over Southeast Asia,
The height of the tropopause • During the summer monsoon, the tropopause occasionally peaks above 18 km. • In other words, cold conditions lead to a lower tropopause, obviously because of less convection.
The height of the tropopause • Deep convection (thunderstorms) in the Intertropical Convergence Zone, or over mid-latitude continents in summer, continuously push the tropopause upwards and as such deepen the troposphere. This is because thunderstorms mix the tropospheric air at a moist adiabatic lapse rate.
The height of the tropopause • In the upper troposphere, this lapse rate is essentially the same as the dry adiabatic rate of 10K/km. So a deepening by 1 km reduces the tropopause temperature by 10K. Therefore, in areas where (or at times when) the tropopause is exceptionally high, the tropopause temperature is also very low, sometimes below -80� C.
The height of the tropopause • Such low temperatures are not found anywhere else in the Earth's atmosphere, at any level, except in the winter stratosphere over Antarctica.
