Abstract

The minimum, moderate and maximum temperature trends at seasonal time scale in 5 climatic zones using 37 meteorological stations in Zayandehrud river basin was studied regionally and the relationship to water resources, water uses of each zone and its possible effects were determined. The results showed that the majority of the climatic zones will have an increasing trend in spring, summer and fall and a decreasing trend in winter. The highest growth rate occurs in overnight temperature in spring and summer and daily temperature in fall. In winter, there is no significant difference between the slopes of temperature variables trend. The Most increasing slopes of the trend are seen in the northern part of the basin and during summer and the least decreasing slopes are in the northern and North-western parts of the basin during winter. The temperature rise in fall, spring and summer affect the reduction of water resources and increasing consumption in different areas. Among the various zones, the Eastern part of the basin will be faced with more water stress to meet their needs. The findings of this study can be effective for an identification of sensitive areas to climate change in the basin and planning to control water stress and achieving sustainable river basin management. Cloud coverage and rainfall associated defectively with the subtractive temperature span. Detailing long-term tendencys or determined moves in temperature and precipitation is significant for considerate the present and future alterations in nature. Monthly precipitation alterations may be optimistic or undesirable in various months of the year. While heating can possibly abridge the crop growth period, crop production and water efficiency of all crops are anticipated to reduction due to lower precipitation and higher water prerequisites under higher temperature. The Zayandeh-Rud River basin, Iran, is anticipated to encounter spatiotemporally heterogeneous temperature rise and precipitation decrease that will reduction water supply by mid-century. consequences propose that infrastructural recoveries, strict water request management and ecosystem-based regulatory prioritization, integrated by supply increase can temporarily reduce water stress in a basin.

Highlights

  • Greenhouse gas emission is rising due to the industrial revolution in the world from the 1900s

  • Wang et al (2012) studied trend in annual temperatures and precipitation variations for a 50-year period in Loess Plateau Region (LPR) and showed that the average temperature of the region increased by 1.91°C during this period

  • Grieser et al (2002) studied temperature pattern in Europe during the 100-year period and the results showed a downward trend in annual temperature in Western Europe and incremental trend in Eastern Europe

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Summary

Introduction

Greenhouse gas emission is rising due to the industrial revolution in the world from the 1900s These gases prevent heat resulting from solar radiation reflected from the Earth's surface into space that will cause changes in energy balance and the gradual increase of global temperature (Takara et al, 2009). Martinez et al (2010) studied daily and nightly temperature trend using 37 stations date in the region of Catalonia (Spain) in the period 1975-2004 They showed the annual temperature has increased at an average of 0.5°C per decade and this increase occurred especially in summer and spring. Ahmed et al (2014) evaluated trends of maximum and minimum temperatures for the period 1941–2005 in Ontario, Canada According to their results, maximum temperature is rising in the seasonal and annual scale. They found a significant positive trend for Malta, Jerusalem and Tripoli at the 99% confidence level and a negative trend for Amman at the 95% confidence level

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