The Weather and Climate of Istanbul, Turkey
Wednesday, December 14, 2011
Wednesday, December 7, 2011
Climate Comparison: Istanbul, Turkey and Buenos Aires, Argentina
Thursday, December 1, 2011
Past, Present, and Future of Istanbul, Turkey
Present
(Current World Map, Source: lib.utexas.edu)
In order to effectively compare Turkey of the past with Turkey of the future a base line should be clearly defined. That means just a little recap of modern Turkey and its characteristics. Turkey is located in between the Mediterranean Sea and the Black Sea at about 39˚N and 35˚E. It is classified as having a mostly Mediterranean climate with hot, dry summers and mild, wet winters. Current air masses that affect this area include the Asian High and several Mediterranean Lows. Because of the midlevel latitudes, Turkey has fairly variable weather throughout the year. There are very distinct seasons but nothing too extreme.
(Climograph for current day Istanbul, Source: istanbul.climatetemp.info)
There is moderate variation in temperature and precipitation, thanks to its latitude and regional air masses.
100 Million Years in the Past
(Earth 100 million years ago, Source: ncdc.noaa.gov)
In the not so distant geologic past, 100 million years or so, Turkey was under water. This could be because the ice caps were holding less water and the oceans were at higher levels. It was also about 10˚ closer to the equator in latitude because of tectonic forces. Both of these factors have major impacts on the region’s weather and climate. Because the country is underwater, I will just focus on the land nearby and the area as a whole. Much like where it is now, the region is centered on a small sea. This one was a little bigger than the Mediterranean Sea, near where Istanbul is now. I think in the past Istanbul was a fair comparison with Muscat, Oman. Muscat is on the coast of the Indian Sea and at around 30˚ latitude, much like 100 million-year-old Turkey. Using that comparison I would expect old Turkey to be a very turbulent place being so close to the ITCZ and large bodies of water. I would also expect a climograph to be very similar to the one below.
(Modified climograph of Muscat, Oman to represent Turkey 100 million years ago, Source: climatetemp.info)
I think this is a good representation of old Turkey because it shows the less variable, warmer temperatures, as the region was much closer to the equator. This would lead to higher levels of insolation and the area would absorb more solar energy. For Turkey itself, being underwater and all, it would retain a lot of that energy because water heats and cools slower than land. This process also explains the little variation in temperatures.
100 Million Years in the Future
(Estimated map of Earth 150 million years in the future, Source: scotese.com)
As the tectonic plates continue to shift and move Africa was smash into where Turkey currently resides. As it pushing up into Europe the Mediterranean Mountains will be formed and Turkey will sit right on top. Also, the whole region will move farther north. Having always been near water, this new location will drastically alter Turkey’s weather and climate. It will find itself land locked and, for the first time, dealing with continentality. Also, the higher latitude will greatly change the current air masses affecting the area.
(Modified climograph for Moscow, Russia to represent Turkey 100 year in the future, Source: climatetemp.info)
This modified climograph of Moscow, Russia serves as a fairly good estimation for the weather and climate of new Turkey. Like Moscow, Turkey will be a landlocked subarctic region with very high temperature variation throughout the year and fairly low precipitation. However, unlike Moscow, new Turkey will have a very high elevation that may cause greater precipitation but if I were to guess I would predict a good majority of Turkey would be covered in new glaciers, as the pattern of melt/thaw continues. Of course, in order for glaciers to develop snow must fall.
Wednesday, November 30, 2011
Climatology
POTENTIAL IMPACTS OF CLIMATE CHANGE ON AGRICULTURE IN TURKEY by Levent Saylan, PhD.
CLIMATOLOGICAL APPLICATIONS IN TURKEY by Serhat Sensoy
Monday, November 7, 2011
Istanbul, Turkey vs. Shanghai, China
For one, Istanbul sits at about 288 m (945 ft) where Shanghai, built on an alluvial fan, has a measly 5 m (13 ft). As we have learned in class, elevation is a major factor of weather, as air cools as it rises. This means that the air in Istanbul is, on average, colder than the air in Shanghai. This impacts how much moisture air-masses can carry over these areas, as well as dew point levels and other precipitation elements.
Another interesting comparison is that the weather of both cities is actually influenced by the same semi-permanent high-pressure system that develops over Asia, only in different ways. The Siberian Anti-Cyclone (Or Continental Asian High) rotates clockwise over mainland Asia, bringing rain to Istanbul and the dry season for Shanghai. The easterly winds from the lower-left part of the system blows air across the Black Sea into Istanbul, causing that area’s wet season. By the time the system travels across all of Asia and gets to Shanghai, on the other side of the high, the northwesterly winds have been drained of their moisture. So while both cites are affected by the same system they experience entirely different conditions.
Of course, this pressure system is not year round and during its absence the weather in both cities swap. As stated in the last blog, when the high is over mainland Asia a number of low systems develop around Istanbul, thus all the rain. When the Asian high dissipates so do the lows over Istanbul and the weather mellows and becomes more temperate. However, in Shanghai, when the high moves out lows move in and their monsoon season begins. Looking at the two graphs above you can see how the wet season in Shanghai follows almost immediately after the rainy season in Istanbul and that the relative humidity of both cities are inverted.
Sources:
http://shanghiweatherandclimate.blogspot.com/
http://en.wikipedia.org/wiki/Istanbul
Wednesday, October 19, 2011
Air Masses and Moisture
(Path of the March solar eclipse with Turkey in red - Source: http://eclipse.gsfc.nasa.gov)
Aiding in this movement are the several Mediterranean Lows. According to NASA there are a number of locations in the Mediterranean area that a common “sinks” of low-pressure systems. One of which just so happens to reside directly over Istanbul. This system usually develops in the string months but can be seen all year. It is this combination of the Siberian High, Mediterranean Lows, and the two seas that drives Istanbul’s weather and precipitation.
(Climate Classification for Turkey - Source: www.atc-anadolu.com)
The map above shows Istanbul classified as having a “humid” climate. Knowing its location and air patterns this seems perfectly reasonable.
(Precipitation for Turkey (mm) - Source: www.atc-anadolu.com)
Sources:
http://eclipse.gsfc.nasa.gov/SEpubs/20060329/text/section2.html
www.britannica.com/EBchecked/topic/372680/Mediterranean-low