Fractal-multifractal ensembles of downscaled precipitation and temperature sets as implied by climate models

Author(s):  
Mahesh Lal Maskey ◽  
David Joseph Serrano Suarez ◽  
Joshua H. Viers ◽  
Josue Medellin-Azuara ◽  
Bellie Sivakumar ◽  
...  

<p>Describing the specific details and textures implicit in real-world hydro-climatic data sets is paramount for the proper description and simulation of variables such as precipitation, streamflow, and temperature time series. To this aim, a couple of decades ago, a deterministic geometric approach, the so-called fractal-multifractal (FM) method,<sup>1,2</sup> was introduced. Such is a holistic approach capable of faithfully encoding (describing)<sup>3</sup>, simulating<sup>4</sup>, and downscaling<sup>5</sup> hydrologic records in time, as the outcome of a fractal function illuminated by a multifractal measure. This study employs the FM method to generate ensembles of daily precipitation and temperature sets obtained from global circulation models (GCMs). Specifically, this study uses data obtained via ten GCM models, two sets of daily records, as implied from the past, over a year, and three sets projected for the future, as downscaled via localized constructed analogs (LOCA) for a couple of sites in California. The study demonstrates that faithful representations of all sets may be achieved via the FM approach, using encodings relying on 10 and 8 geometric (FM) parameters for rainfall and temperature, respectively. They result in close approximations of the data's histogram, entropy, and autocorrelation functions. By presenting a sensitivity study of FM parameters' for historical and projected data, this work concludes that the FM representations are useful for tracking and foreseeing the records' complexity<sup>6</sup> in the past and the future and other applications in hydrology such as bias correction.</p><p> </p><p> </p><p><strong>References</strong></p>

2019 ◽  
Vol 25 (85) ◽  
pp. 64-88
Author(s):  
Janez Juvan

Abstract The article presents research on the international community’s engagement in the countries of the Western Balkans in the past and their possible approach in the future. The focus of our research is on the functioning of mechanisms through which the international community performs certain tasks in the region. These interventions are primarily political, in the form of conferences, political programmes, consultations, pressures and continuous persuasion. Economic initiatives follow afterwards. By using different reform approaches, international institutions try to improve cooperation with the European Union (EU) and countries such as the USA, Russia, Turkey and China. Our research attempts to identify possible methods and new solutions for individual cases of conflict in Western Balkans countries, especially where the international community is actively involved. On this basis, we created a more holistic approach. The application of these measures could make the necessary reforms of the future easier. Our approach emphasises all the elements of security that are essential to the stability of the region and for the prevention of conflicts in the future.


1993 ◽  
Vol 20 (3) ◽  
pp. 223-226 ◽  
Author(s):  
Hassan A. Nasrallah ◽  
Robert C. Balling

Within the past few years, interest in climate change has increased dramatically in the face of the many apocalyptic predictions associated with the highly-popularized ‘greenhouse’ effect. Accordingly, scientists have produced many studies based on global, hemispheric, and regional, climatic data-bases. While most of the regional studies have been based on data from North America, Europe, and Australia, little research has been conducted in other areas of the world that have an equal (or greater) economic and climatic stake in the ‘greenhouse’ debate. In this investigation, we analyse the climatic records of the Arabian Gulf area in an attempt to identify recent changes that may or may not be related to any ‘greenhouse’ effects.The observed climate changes over the past century in the Arabian Gulf area include (a) an increase in temperature of 0.65°C, (b) warming in summer and little or no warming in winter, (c) no warming in the first 60 years of record but accelerated warming in the most recent 40 years, and (d) a small decline in precipitation. In many cases, the results are unlike those found in the analysis of Northern Hemispheric and/or global climate records. However, many of these observed climate changes in the Arabian Gulf area are broadly consistent with 2×CO2 predictions from various numerical climate models. We hope that the analyses presented in this investigation will aid decisionmakers in their difficult policymaking activities.


2009 ◽  
Vol 22 (8) ◽  
pp. 2181-2198 ◽  
Author(s):  
Tessa Sou ◽  
Gregory Flato

Abstract Considering the recent losses observed in Arctic sea ice and the anticipated future warming due to anthropogenic greenhouse gas emissions, sea ice retreat in the Canadian Arctic Archipelago (CAA) is expected and indeed is already being observed. As most global climate models do not resolve the CAA region, a fine-resolution ice–ocean regional model is developed and used to make a projection of future changes in the CAA sea ice. Results from a historical run (1950–2004) are used to evaluate the model. The model does well in representing observed sea ice spatial and seasonal variability, but tends to underestimate summertime ice cover. The model results for the future (2041–60) show little change in wintertime ice concentrations from the past, but summertime ice concentrations decrease by 45%. The ice thickness is projected to decrease by 17% in the winter and by 36% in summer. Based on this study, a completely ice-free CAA is unlikely by the year 2050, but the simulated ice retreat suggests that the region could support some commercial shipping.


2011 ◽  
Vol 8 (5) ◽  
pp. 9005-9062 ◽  
Author(s):  
D. T. Mengistu ◽  
A. Sorteberg

Abstract. The hydrological model SWAT was calibrated with daily station based precipitation and temperature data for the whole Eastern Nile basin including the three subbasins: the Blue Nile, Baro Akobo and Tekeze. The daily and monthly streamflow was calibrated and validated at six outlets in the three different subbasins. The model performed very well in simulating the monthly variability of the Eastern Nile streamflow while comparison to daily data revealed a more diverse performance for the extreme events. Of the Eastern Nile average annual rainfall it was estimated that around 60% is lost through evaporation and estimated runoff coefficients were 0.24, 0.30 and 0.18 for Blue Nile, Baro Akobo and Tekeze subbasins, respectively. About half to two-thirds of the runoff could be attributed to surface runoff while the remaining contributions were from groundwater. The annual streamflow sensitivity to changes in precipitation and temperature differed among the basins and the dependence of the response on the strength of the changes was not linear. On average the annual streamflow responses to a change in precipitation with no temperature change was 19%, 17%, and 26% per 10% change in precipitation while the average annual streamflow responses to a change in temperature and no precipitation change was −4.4% K−1, −6.4% K−1, and −1.3% K−1 for Blue Nile, Baro Akobo and Tekeze river basin, respectively. While we show the Eastern Nile to be very sensitive to precipitation changes, using 47 temperature and precipitation scenarios from 19 AOGCMs participating in IPCC AR4 we estimated the future change in streamflow to be strongly dependent on the choice of climate model as the climate models disagree on both the strength and the direction of future precipitation changes. Thus, no clear conclusions can be made about the future changes in Eastern Nile streamflow.


2021 ◽  
Author(s):  
Paolo Scussolini ◽  
Pepijn Bakker ◽  
Paolo De Luca ◽  
Dim Coumou ◽  
Joyce Bosmans ◽  
...  

<p>Past climates contain precious information about the workings of the climate system, and about what can be expected in a changed climate. The Last Interglacial (LIG; ca. 125,000 years ago) is the most recent period of climate warmer than modern, at least in the Northern Hemisphere. Because of this, it has been often proposed that the LIG holds a partial analogy with a future warmer climate forced by enhanced greenhouse effect. Still, such analogy has never been examined in a quantitative manner. Here we address the question: for which scenario, time horizon, regions and season is the climate of the LIG a useful analogue of the future? We use the results of 13 climate models that performed the standard experiments of PMIP4 and CMIP6, and present a comparison of hemispheric temperature and precipitation between the LIG and SSP scenarios of the future. We also two independent assessments of models performance, by comparing their temperature and precipitation to climate reanalysis of the last decades and to proxies of the LIG. Insights gained from this comparison can inform studies in disciplines beyond climate studies, such as hydrology and ecology.</p>


1980 ◽  
Vol 25 (3) ◽  
pp. 230-231
Author(s):  
MARCEL KINSBOURNE
Keyword(s):  
The Past ◽  

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