எங்கள் குழு ஒவ்வொரு ஆண்டும் அமெரிக்கா, ஐரோப்பா மற்றும் ஆசியா முழுவதும் 1000 அறிவியல் சங்கங்களின் ஆதரவுடன் 3000+ உலகளாவிய மாநாட்டுத் தொடர் நிகழ்வுகளை ஏற்பாடு செய்து 700+ திறந்த அணுகல் இதழ்களை வெளியிடுகிறது, இதில் 50000 க்கும் மேற்பட்ட தலைசிறந்த ஆளுமைகள், புகழ்பெற்ற விஞ்ஞானிகள் ஆசிரியர் குழு உறுப்பினர்களாக உள்ளனர்.
அதிக வாசகர்கள் மற்றும் மேற்கோள்களைப் பெறும் திறந்த அணுகல் இதழ்கள்
700 இதழ்கள் மற்றும் 15,000,000 வாசகர்கள் ஒவ்வொரு பத்திரிகையும் 25,000+ வாசகர்களைப் பெறுகிறது
Yassine Charabi
Oman is one of most water-stressed countries in the world. Therefore, keeping water and energy supply and demand in equilibrium in a pressing development is a challenge facing Oman in the years ahead. The threat from the potential impacts of climate change has growing with the recent tropical cyclones that had affected the country and caused loss of life and substantial damage throughout the coastal areas of Oman. The design of an effective climate change strategy requires a deep knowledge about the past, the present climate and also requires an accurate estimation of the plausible change in future climate. This paper presents a rather complete picture about the current (1961-1990) and future (2011-2070) projection of the pattern of rainfall and temperature. For the assessment of the future climate projection over Oman, the 21st century the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4) A1B, forcing scenario is used with the climate model of the National Center for Atmospheric Research (NCAR) and the Community Climate System Model (CCSM-3). The A1B scenario clearly shows future minimum temperature increases that are in line with the results shown that minimum temperatures will experience the greatest impact from climate change. The simulation shows that the northern of Oman is expected to face decreasing rainfall in the coming decades. In a region where historic average annual rainfall levels are between 50 and 100 mm for the northern coast area, climate change is expected to lead to between 20 and 40 mm less rainfall by 2040. This is equivalent to a reduction in average annual rainfall of about 40%. With less future rainfall in northern areas, groundwater recharge, surface water flow and water quality are expected to also decrease.