پديد آورندگان :
قويدل رحيمي، يوسف دانشگاه تربيت مدرس - گروه جغرافياي طبيعي , فرج زاده اصل، منوچهر دانشگاه تربيت مدرس - گروه جغرافياي طبيعي , عالي جهان، مهدي دانشگاه تربيت مدرس
كليدواژه :
حساسيت پذيري , گرمايش جهاني , دماي متوسط , آزمون من - كندال , ايران
چكيده فارسي :
اگر چه وجود يا عدم وجود تغيير اقليم جاي بحث دارد، اما تقريباً همه اقليم شناسان گرمايش جهاني را به عنوان يك معضل و مخاطره اقليمي قبول دارند. به دليل اهميت اين موضوع، پژوهش پيش رو جهت ارزيابي ميزان تاثير گرمايش جهاني بر روي دماهاي متوسط، به صورت ماهانه و دوره اي (سرد و گرم) انجام گرفته است. براي انجام اين پژوهش از دو دسته داده، داده هاي دماي 17 ايستگاه سينوپتيك كشور و مقادير متناظر آن، داده هاي شاخص ناهنجاري هاي متوسط دمايي خشكي ها و اقيانوس هاي كره زمين طي بازه زماني 60 ساله (2010-1951) ميلادي استفاده شده است. جهت انجام اين پژوهش از روش همبستگي پيرسون براي محاسبه ارتباط بين داده ها، از روش روند خطي جهت تحليل مولفه روند سري زماني داده ها، براي نشان دادن پراكندگي مكاني همبستگي بين داده هاي دماي ايستگاه ها با گرمايش جهاني در سطح كشور از مدل زمين آمار و در نهايت جهت تشخيص معناداري روند تغيير دماها از آزمون ناپارامتري من – كندال استفاده گرديده است. با توجه به نتايج بدست آمده همه ايستگاه هاي مطالعاتي به غير از اروميه و خرم آباد روندي افزايشي در دماي متوسط را تجربه مي كنند. بيش ترين تاثير گرمايش جهاني از ماه آوريل تا اكتبر مشاهده مي گردد كه در اين بين ماه هاي تابستان نسبت به ساير ماه ها از ضريب همبستگي بالاتري برخوردار بوده و نشان از افزايش دماي متوسط تابستانه دارد. فرآيند ذكرشده در بررسي هاي تحليل سري زماني و تغيير روند دمايي صورت گرفته نيز كاملاً مشهود بوده و تغير روند صورت گرفته در بيشتر ماه ها كاملاً معني دار بوده و تغير در روند دماي متوسط صورت گرفته را تصديق مي كند. نتايج حاصل از تحليل هاي رابطه دماي متوسط دوره هاي سرد و گرم با شاخص ناهنجاري هاي متوسط دمايي خشكي ها و اقيانوس هاي كره زمين گوياي رابطه معنادار قوي دوره گرمايي نسبت به دوره سرد است. تغير روند دمايي صورت گرفته در هر دو دوره مطالعاتي براساس نتايج حاصله كاملاً معنادار مي باشند.
چكيده لاتين :
Although it is questionable whether there is climate change, but almost all
climatologists agree that global warming is a problem and that climate hazard. In
history before the Industrial Revolution, Earth's climate changed due to natural
causes not related to human activity. Most often, global climate has changed because
of variations in sunlight. Tiny wobbles in Earth's orbit altered when and where
sunlight falls on Earth's surface. Variations in the Sun itself have alternately increased
and decreased the amount of solar energy reaching Earth. Volcanic eruptions have
generated particles that reflect sunlight, brightening the planet and cooling the
climate. Volcanic activity has also, in the deep past, increased greenhouse gases over
millions of years, contributing to episodes of global warming. "Global warming" refers to the global-average temperature increase that has been observed over the last one
hundred years or more. But to many politicians and the public, the term carries the
implication that mankind is responsible for that warming. Global warming occurs
when water vapors and other greenhouse gasses collect in the atmosphere and
absorb sunlight and solar radiation that have bounced off the earth's surface.
Normally, this radiation would escape into space-but these pollutants, which can last
for years to centuries in the atmosphere, trap the heat and cause the planet to get
hotter. That's what's known as the greenhouse effect. The impacts of global warming
are being felt across the globe. Extreme heat waves have caused tens of thousands of
deaths around the world in recent years. And in an alarming sign of events to come,
Antarctica has been losing about 134 billion metric tons of ice per year since 2002.
Over the past 50 years, the average global temperature has increased at the fastest
rate in recorded history. And experts see the trend is accelerating: All but one of the
16 hottest years in NASA's 134-year record have occurred since 2000.
Each year, scientists learn more about the consequences of global warming, and
many agree that environmental, economic, and health consequences are likely to
occur if current trends continue. Here's just a smattering of what we can look
forward to:
- Melting glaciers, early snowmelt, and severe droughts will cause more dramatic
water shortages and increase the risk of wildfires in the American West.
- Rising sea levels will lead to coastal flooding on the Eastern Seaboard, especially in
Florida, and in other areas such as the Gulf of Mexico.
- Forests, farms, and cities will face troublesome new pests, heat waves, heavy
downpours, and increased flooding. All those factors will damage or destroy
agriculture and fisheries.
- Disruption of habitats such as coral reefs and Alpine meadows could drive many
plant and animal species to extinction. -Allergies, asthma, and infectious disease outbreaks will become more common due
to increased growth of pollen-producing ragweed, higher levels of air pollution, and
the spread of conditions favorable to pathogens and mosquitoes.
Air temperature is the most sensitive meteorological element to global warming.
Because of this, the research ahead is done for the detection of global warming on
average temperatures in monthly and periodic (hot and cold) time scales.
- Data Methods
For this study, two groups of data, monthly average temperatures data of 17 synoptic
stations and corresponding amounts of data in global land and oceans temperature
anomalies were figured out over 60 years period of time (1951 to 2010}. Goals, the
Pearson correlation method for detecting relationships between data's, and linear
trend for trend analysis time series data, To illustrate the correlation between the
spatial distribution of temperature data with global warming stations nationwide
Geostatistical model Finally, non-parametric test for detecting significant
temperature changes Man - Kendall method were used.
Discussion and Conclusion
According to the results, all studies stations apart from Urmia and Khorramabad
experience increasing trend in the average of temperature. The most influence over
global warming observed from April to October is the month of the summer than
other months of the relationship that has a significant high than the average summer
temperature is going up. This process in the analysis of time-series and temperature
trends has been quite evident. Change in trend occurred been a significant in most
months and changes in the average temperature trend has been confirmed. The
results obtained from the analysis period (hot and cold) temperatures average,
indicating a strong relation to the hot period than the cold periods. The change in temperature trend occurred in both studies period, According to the results obtained
are quite significant.
Conclusions
This study investigated the statistical characteristics and spatiotemporal distribution
and trends of average temperatures events and its relationships to global land ocean
anomalies in Iran. According to obtained results in summer months and hot period
relationships between average temperatures of stations and global land ocean
anomalies are significant than other seasons and months. Therefore global warming
is affected on average monthly temperatures of Iran.