نتایج جستجو برای: g a2 and hadcm3 a1b
تعداد نتایج: 16876331 فیلتر نتایج به سال:
introduction today, climate change issue is one of the main challenges for scientists and due to the critical role of water in human life, the study of climate change impacts on severity and frequency of drought in each region seems to be indispensable (hulme et al., 1999). drought is usually occurred over a period of water shortage owing to less rainfall, high evapotranspiration and pumping a ...
Climate change is an unprecedented change are taking place. Changes of meteorological parameters such as precipitation, maximum and minimum temperatures. Since weather forecasting is important for these parameters, in this study, the performance of Statistical Downscaling Model (SDSM and Lars-WG) were used to predict temperature and precipitation and mean of these changes for the periods 2046-2...
Climate change due to increasing the concentration of greenhouse gases (especially CO2) in the atmosphere causes changes in the rainfall regime, runoff rate, wind speed and solar radiation of atmosphere. In the present research, the maximum and minimum temperature parameters were simulated during the base period of 1979-2088 and two future periods of 1979-2070 and 2070-2090 using daily ...
افزایش غلظت گازهای گلخانه ای در جو زمین تغییرات قابل ملاحظه ای را در اقلیم زمین به وجود آورده است. با توجه به اینکه گرمایش زمین عامل تهدید کننده ای برای زندگی بشر و کشاورزی در کره زمین می باشد، لذا پیش بینی تغییرات اقلیمی در آینده امری ضروری به حساب می آید. تغییر در الگوی بارش، دما و سایر متغیرهای اقلیمی بر رژیم هیدرولوژیکی نواحی مختلف تأثیرگذار است. مدل های جهانی اقلیم gcm مهمترین منبع برای دس...
امروزه تغییر اقلیم اثرات انکارناپذیری بر کلیه ی بخش ها بخصوص بخش کشاورزی دارد. بررسی و ارزیابی اثرات اقتصادی ناشی از تغییر اقلیم بر این بخش می تواند موجب بهبود و توسعه راهبردهای مدیریتی شده و سبب کاهش اثرات سوء تغییر اقلیم در این بخش گردد. در این مطالعه سعی شد تا با تبیین تئوریک و طراحی یک مدل در قالب رهیافت ریکاردین و با استفاده از تکنیک داده های پانل به دو روش ایستا و پویا که به ترتیب مبتنی ب...
[1] Observations and simulations (using the HadCM3 AOGCM) of time-dependent twentieth-century climate change indicate a linear relationship F = rDT between radiative forcing F and global mean surface air temperature change DT. The same is a good description of DT from CMIP3 AOGCMs integrated with CO2 increasing at 1% per year compounded. The constant ‘‘climate resistance’’ r is related to the t...
We present results of an implementation of the Elastic Viscous Plastic (EVP) sea ice dynamics scheme into the Hadley Centre coupled ocean-atmosphere climate model HadCM3. Although the large-scale simulation of sea ice in HadCM3 is quite good with this model, the lack of a full dynamical model leads to errors in the detailed representation of sea ice and limits our confidence in its future predi...
The contribution to sea level to 2200 from the grounded, mainland Antarctic Peninsula ice sheet (APIS) was calculated using an ice-sheet model initialized with a new technique computing ice fluxes based on observed surface velocities, altimetry and surface mass balance, and computing volume response using a linearized method. Volume change estimates of the APIS resulting from surface massbalanc...
Temperature, precipitation and wind extremes over Europe are examined in an ensemble of RCA3 regional climate model simulations driven by six different global climate models (ECHAM5, CCSM3, HadCM3, CNRM, BCM and IPSL) under the SRES A1B emission scenario. The extremes are expressed in terms of the 20-yr return values of annual temperature and wind extremes and seasonal precipitation extremes. T...
The Influence of Climate Change on Winter Wheat during 2012–2100 under A2 and A1B Scenarios in China
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