Abstract
Daily and overnight temperature trends in annual time-scale for Zayanderud river basin using 37 meteorological stations were studied. According to the results the majority of trends in the time series of daily and overnight temperature were increasing. Warming trends in the overnight temperature were stronger than those in the daily temperature. The average of all stations in the daily and overnight trends was 0.003 and 0.014C year−1 respectively. Overall warming trends (daily-overnight) were consistent with increasing urbanization. Regional warming trends were more obvious in the more urbanized area in central and eastern basin. There were weak cooling trends in daily temperature in the western and southwestern basin with a colder and more rainfall climate.
Highlights
This glance inspects the straight results of climate change on the environment
21 out of 37 stations have increasing trend, 14 stations have experienced decreasing trend and 2 stations are without trend but only the increasing trend of the Tiran station is significant
Warming trends vary between 0.001-0.020 C year−1 at
Summary
This glance inspects the straight results of climate change on the environment. Temperature is identified as the prevailing abiotic component instantly affecting Environmentals. Temperature immediately affects progress, durability, range and amplitude. The primary result of temperature in temperate areas is to impact winter survival; the two components do not presently do in tandem. The World Health Organization approximates that the warming and precipitation movements due to anthropogenic climate change. Doubt stays in assigning to the development to climate change, owing to lack of long-time, high-quality data sets as well as the large impact of socio-economic components and alters in invioability. Air modality is forcefully related on weather and is touchy to climate change. We inspect these various ways and their consequences. The later climate is anticipated to be more static, owing to a weaker global circulation and a reducing alternation of mid-latitude cyclones
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