AN INVESTIGATION INTO THE QUALITATIVE AND QUANTITATIVE EFFECTS OF CLIMATE CHANGE ON RIVERS IN IRAN Hojat Dehghani Vahid 1, Mohammad Noori 2*, Mohammad Heydari 3, Mohammadsaeid Sheikhi 4 1. MSc student, LameiGorgani institute of higher education, Gorgan, Iran 2 PhD of Civil engineering, Ferdowsi university of Mashhad, Mashhad, Iran 3. PhD candidate, University Malaya, Kuala Lumpur, Malaysia 4. MSc student, LameiGorgani institute of higher education, Gorgan, Iran Abstract The climate change phenomenon has had a negative effect on agriculture, environment and different water resource systems, especially in rivers due its impact on climatic factors such as rainfall, temperature and solar radiation. Ignoring climate change studies in the hydraulic systems designs will cause severe implications. Even a minor change in hydraulic variables will lead to tangible changes in the water resources system operation. Therefore, the effects of climate change on rivers have been briefly studied with a conceptual point of view. Keywords: Climate Change, Water Resources, River Basin, Land Use, Climate Variability, Hydrological Modeling. 1 Background An increasing trend of the earth’s temperature and changes in the associated global weather conditions is known as climate change [1]. Due to worldwide development, climate studies have become even more challenging. The greenhouse gases are known as the major driver of current climate change, and this has caused numerous problems that have affected different parts of the world. Following the significance of the climate change issue resulted from human activities, it has become more necessary than ever to conduct studies that identify and reveal climate change. Currently, some studies are being conducted on climate parameters and their enormous effects to find the causes of these changes. Some research is also done to provide a good insight of natural- social [2, 3], economic system [4, 5] and its sensitivity to climate change. Also, in Iran, many studies have been conducted on climate change and its effects on various factors [6-8]. Below, the climate parameter trends such as temperature, rainfall, wind, humidity, etc. have been evaluated in Iran from 1951 to 2005. Recently, attention has been drawn to analyzing the time series of rainfall, temperature, sunshine hours, etc. in order to investigate climate parameters [9]. 2 2.1 The trend of changing climate parameters in Iran Temperature The increment of minimum temperature and maximum temperature are studied and evaluated in a significant number of stations in Iran. The overall trend of minimum temperature compared to the normal period of 1961-1990 has been demonstrated in the 19512005 period as shown in Figure 1. This figure proves the temperature increase in Iran. Changes in the minimum annual temperature ( C°) Reducing the range of boarding changes is very prominent in most areas of Iran, for example, in Figure 2 this range has been provided in the form of its difference of normal period from 1961- 1990. Overall, considering the process of extent profiles of temperature in Iran from the second half of the twentieth century indicates the increasing frequency of warm events such as warm days, and the reducing frequency of cold events such as freezing days. It should be mentioned that most of the obtained results are consistent with the results gained by interstate board of climate change and other collective studies. Year Fig1. The process of minimum temperature in Iran from 1951 to 2005 compared to the normal period Fig 2. Changing trend of temperature 2.2 Rainfall The rainfall average trend in Iran has been negative from the beginning of the second century until now. Figure 3 demonstrates the process of precipitation profiles in all static modes in the country. As an overall conclusion, it can be asserted that a considerable part of the research findings are mainly consistent with the interstate board of climate change. Fig 3. Decadal trend of rainfall in period 1951- 2005 2.3 Wind As outlined in Figure 4, the annual average of wind speed for the period of 1951 to 2005 is at a decreasing trend. This reduction is perhaps due to effective factors such as the city’s expansion, structural changes in their surroundings, precipitation pattern changes and other atmospheric elements. It should be noted that factors like the reduction of wind speed, increasing population and urban development will cause a potential pollution increase in the cities of Iran. Fig 4. The annual average of wind speed trends from 1951 to 2005 2.4 Humidity Through global warming, we encounter an increase in humidity in the air along with temperature increase in many parts of the world. In order to determine the level of humidity, the dew point temperature trend is considered a good benchmark. The linear process of dew points at two stations is provided in Figures 5 and 6 as samples. Fig 5. Dew point temperature trend from 1951 to 2005 compared with the normal period from 1961 to 1990 Fig 6. Dew point temperature trend in the period 1951- 2005 compared with the normal period of 1961-1990 3 Effects of climate change on river Human lives have always been subjected to different natural risks all over the world. Parts of these dangers have mainly been due to the climate change processes such as flood, drought and severe storm events. These dangers are relatively more widespread and frequent [10]. Nowadays the impact of climate changes on water resources is obvious, especially on rivers. The surface water or rivers are the most crucial water resources which have a main role in supplying water required for different activities such as agriculture, industry, consumption and electricity production [11]. Climate changes can affect different aspects of rivers. Among the areas that are affected by climate change are some factors like hydrological factor, water quality, ecosystems, soil erosion and sedimentation. 3.1 The hydrological factors and floods The effect of climate change on the hydrologic plan and management of hydro systems could be one of the significant challenges faced by future practicing hydrologists and water resource administrators [12]. Flooding of rivers has caused many human and financial losses. The risks have also increased due to climate changes and human interference to the river systems in recent times [13]. It seems that by increasing temperature and evaporation, reducing precipitation, the flood extent has been reduced, but investigations conducted in the past shows a different result that proved the opposite was true, because by reducing the runoff volume, there will be a reduction in maximum flow rate of discharge, which is one of the important reasons of climatic change. Studies have shown that the number of floods occurred is approximately fifty times. It proves the accuracy of the contents. Moreover, the hot weather is able to preserve more humidity, and will increase the evaporation of the wet surfaces. Increasing the humidity in the atmosphere will lead to the aggravation of snow precipitation and rainfall events and the increasing potential of higher river levels and the occurrence of floods. 3.2 Discharge The first step in water project engineering studies is the correct use of data and information [14]. Appropriate estimation of watershed discharge has been discussed by the specialists in a variety of construction projects and this significant issue has considerable impact on the design of the required structures [15]. According to the obtained information, in the spring, the reduction of snow melting and the increase in air temperature reduces the river discharge. This means that generally, an increase in weather temperature causes considerable changes. In mountainous and cold areas, a rise in temperature can somewhat cause snow melting, but increasing the river flow cannot lead to considerable changes. Table 1. The impact of climate change on river discharge Occurrence Impacts Increase the air temperature and changing snow to rain Temperature increment along with increasing evaporation Activity of sunspots Precipitation increment Rainfall increment in warm months along with evaporation Changing the rain to snow in cold months Increasing river discharge in the winter Increasing the temperature and decreasing the winter snow Overall increase in the air temperature The rapid snow melting of and air heat Increasing the temperature and decreasing the precipitation Increasing the time and spatial changes Decrement of the river flow The change in the river course and amount of runoff Increasing the amount of river discharge Reducing the amount of river discharge Reducing the amount of river discharge during the year Maximum flow time transfer of river from spring to winter Increasing the maximum moment discharge of River Changing schedule of flow water production Effective on the peak flow discharge Impact on the flow discharge and flow regime 3.3 Water resources Water is considered as one of the fundamental basis of development, economic prosperity, and social well-being and its shortage will cause many hindrances [16]. Table 2. The impact of climate change on water resources Occurrence Impacts Change of time and spatial distribution of solid and liquid precipitation Meteorological data series and hydrometers heterogeneous Precipitation pattern change Change in hydrometeorology regime of different regions Error in estimating the return period discharge Increasing the temperature along with a change in the amount of precipitation and evaporation Increasing the precipitation and snow melting Increasing the temperature along with evaporation increment and reducing the river flow Warming up the air and reduce the snow in winter and consequently reduction of runoff caused by the melting of snow. Reducing the precipitation and increasing the temperature 3.4 Anomalies in the intensity, duration and amount of precipitation Reducing the duration and continuation of the period time between drought occurrence and outbursts Increasing the runoff high runoff in high latitudes *reducing the runoff and drought increment in low latitudes Increasing the frequency of flood occurrence Change in the rivers regime and surface water reservoirs Dropping off the entrance flow to dams Water quality and ecosystem: Climate change is one of the key factors affecting the quality and quantity of the water in the rivers. The water quality of the river determines the type of its consumption. The elements and effective materials in the quality of the water are different in various discharges; therefore, factors that change the river flow like rainfall, evaporation, temperature will also cause changes in water quality parameters. Generally, in low in dehydration period, due to atmospheric precipitation interruption or little rain, the amount of soluble material in the water increases. During the full-water period the increased discharge of water is along with more rainfall and consequently the concentration of soluble material decreases. According to the type of region, geological studies and determining the chemical characterization of soil, the quality parameters such as electrical conductivity, salinity, total cations and anions and… will be affected and depending on the region will be high or low. Many factors such as dissolved organic matters that their concentration and chemical compound are affected by climate changes and ultra-violet rays, can also affect the penetration depth of ultra-violet rays on natural water. The negative effect of ultra-violet rays on the aquatic insects and water ecosystem is clear to everyone. Solar UV rays penetrate the significant depths of ecology in water systems and affect sweet water and marine systems from the primary producers (Phyto planktons) to consumers (Geo planktons) in the food chain. Table 3. The impact of climate change on water quality Occurrences Impacts Temperature increment along with reducing the precipitation The precipitation increment along with increasing the discharge Reducing the water quality The precipitation decrement The precipitation increment along with the consistent flood occurrence The precipitation increment along with increasing the discharge in the river Increasing the temperature of the weather and the river The precipitation increment Increasing the temperature along with evaporation decrement and flow turbulence increment Reducing the concentration of materials dissolved in water and water quality increment (it may change depending on the research area) Increasing the concentration of material soluble in water Entering more salts into the river and reducing its water quality Reducing the PH of the water and increasing the electrical conductivity Reducing the PH of the water and oxygen dissolved in the water Increasing the suspended solid material in the water Increasing the amount of oxygen *The river flow is the most important factor of water quality control Table 4. The impact of climate changes on the river ecosystem Occurrence Impacts Increasing the UV-B rays Warm and drought climate Increasing the air temperature that causes snow melting in early spring Weather temperature increment and subsequently increasing the water temperature Short term snow in winter and faster snow melting 3.5 *Negative effect on hydraulic ecosystems *The impact of phytoplanktons to Zooplanktons and all nutritional chain Reducing the amount of incoming DOC to rivers Impact on the concentrations and chemical compound of dissolved material Chlorophyll concentration increment Simulating the growth of Phytoplanktons Sedimentation: Climate change may increase the danger of erosion, and the amount of it depends on the environment and regional conditions. Of course, changes in wind and precipitation patterns can affect the rate of erosion. Research has shown that rivers contain different sediments, especially in turbulent conditions. These sediments denote the rate of erosion and transport of materials, and are particularly important in the field studies related to dam construction. The sedimentation level of the rivers has a rational connection with different discharges. Therefore, in regions where the precipitation average increment is along with increasing discharge in rivers, the amount of sediment load of these rivers will increase. These are some of direct and indirect effects of climate change on the river system. Therefore, assessing the impacts of climate change on the River in the coming years can resolve problems such as sudden floods, water quality reduction, reducing the amount of erosion and sedimentation. Table 5. The impact of climate changes in the river sediment Occurrences Impacts Increasing the average of precipitation along with the rivers discharge increment Decreasing the average of precipitation level along with the discharge reduction in rivers The weather temperature, evaporation and transpiration increment and subsequently decreasing the runoff coefficient 3.6 Increasing the amount of sediment load of the rivers, sedimentation and sediment transport increment Decreasing the level of sediment load of the rivers Descending the amount of suspended loads The impact of climate change on erosion: Table 6. The impact of climate changes on the river erosion Occurrence Impacts Precipitation increment along with increasing discharge Climate and precipitation changes resulted from the current climate conditions Displacement in spatial and time cores of the cold weather waves Change in the climate conditions and occurrence of severe storm and precipitation Increasing the river erosion 4 Soil erosions increment and decomposition of organic matter and entering into the river. Increasing the water erosion Loss of vegetation and changing the river bed and privacy. Conclusion: Climate change effects are classified into two groups; direct effects and indirect. Changing the air temperature, precipitation increment, changing the rain to snow in cold months, decreasing the winter snow, the rapid snow melting, increasing the time and spatial changes could be some direct impacts of climate changes. In fact, the indirect effects are the results of direct effects. Increasing or reducing river discharge, anomalies in the intensity, duration and amount of precipitation, changing the amount of suspended soil material in water, changing the PH of water and negative effect on hydraulic ecosystems are known as some samples of indirect climate change effects. In general, the effects of climate change on the river, could be divided into quantity, quality, economical, environmental and social impacts. Hence, in this paper, we studied the trend of changing climate parameters in Iran especially temperature, rainfall, wind and humidity. Furthermore, the climate changes effects on different aspects of rivers such as the hydrological factors and floods, water resources, discharge, water quality and ecosystem and sedimentation were also studied. The findings indicate that climate changes can affect different hydrological and meteorological parameters. Therefore, recognition of these parameters and the amount of their influence can help decision makers to get appropriate policies to combat the challenges of climate change. References: .1 .2 .3 .4 .5 .6 .7 .8 .9 .11 .11 .12 .13 .14 .15 .16 Noori, M., M.B. Sharifi, and M. Heydari. Comparison of the SDSM and LARS-WG weather generators in Modeling of Climate Change in Golestan Province of Iran. in 8th National Congress on Civil Engineering. 2014. Babol Noshirvani University of Technology. Adger, W.N., Social capital, collective action, and adaptation to climate change, in Der klimawandel. 2010, Springer. p. 327-345. Adger, W.N., et al., Are there social limits to adaptation to climate change? Climatic change, 2009. 93(3-4): p. 335-354. Darwin, R., et al., World agriculture and climate change: Economic adaptations. 1995, United States Department of Agriculture, Economic Research Service. Stern, N.H. and H.M.s. Treasury, Stern Review: The economics of climate change. Vol. 30. 2006 :HM treasury London. Abbaspour, K.C., et al., Assessing the impact of climate change on water resources in Iran. Water resources research, 2009. 45(10.) Zarghami, M., et al., Impacts of climate change on runoffs in East Azerbaijan, Iran. Global and Planetary Change, 2011. 78(3): p. 137-146. Kehl, M., Quaternary climate change in Iran—the state of knowledge. Erdkunde, 2009: p. 117. Habibi Khalifeloo, M., M. Mohammad, and M. Heydari, Multiple imputation for hydrological missing data by using a regression method (Klang river basin). International Journal of Research in Engineering and Technology, 2015. 4(6.) Othman, F., et al. Direct and Indirect Effects of Drought using the Function Analysis Systems Technique (FAST) Diagram. in International Conference On Environment (ICENV 2012). 2012. Salarian, M., et al., Classification of Zayandehrud River Basin Water Quality Regarding Agriculture, Drinking, and Industrial Usage. American Research Journal of Civil and Structural Engineering, 2015.)1(1 . Noori, M., et al., Utilization of LARS-WG Model for Modelling of Meteorological Parameters in Golestan Province of Iran. Journal of River Engineering, 2013. 1(1.) ShahiriParsa, A., M. Heydari, and M.A.R.b. Mohd Amiruddin Arumugan. Determination of flood zoning by HEC-RAS model ( Case Study: Johor River - Kota Tinggi Region ). in International Postgraduate Seminar , Organized by Faculty of Civil Engineering , University Teknologi MARA (UiTM). 2013. Habibi Khalifeloo, M., M. Mohammad, and M. Heydari, Application of Different Statistical Methods to Recover Missing Rainfall Data in the Klang River Catchment. International Journal of Innovation in Science and Mathematics, 2015. 3(4.) Fazlolahzade Sadati, S.K., et al., Water Yield Estimation in Polrudwatershed Based on Empirical Methods and Modelling in Geographic Information System (GIS). Journal of river engineering, 2014. 2(7.) Heydari, M., F. Othman, and M. Noori, A review of the Environmental Impact of Large Dams in Iran. International Journal of Advancements Civil Structural and Environmental Engineering, IJACSE, 2013. 1(1): p. 4.