As achievements of the completed United Nations Decade (2005e2014) of Education for Sustainable Development are contemplated globally, along with potential steps forward for the future, Member States have urged that this decade continue after 2014 through "The Future We Want"; the outcome document of the 2012 United Nations Conference on Sustainable Development. More recently, commitments to furthering the advancement of sustainable development through education have also been re-enforced in the recently adopted post-2015 Sustainable Development Goals. This study systematically Barth et al.
This paper aims to study the progress of research on Sustainable Tourism and to outline and identify the key disciplines, journals, articles and authors. This is carried out through a wide, in-depth, and structured examination of published scholarly papers. In recent decades, sustainable tourism has been one of the most significant subjects among academics and practitioners. In this paper, a classification scheme and a comprehensive literature review are presented in order to clarify, categorise, and interpret the current research on sustainable tourism definitions and applications. The classification scheme for this review contains 132 scholarly papers from 47 journals since the year 1993 up to 2013 categorised into 14 application areas. The five major topics are Paradigm, Sustainable Tourism Development, Market research and Economic, Policy-making, and Infrastructure. The scholarly papers are also sorted by (we suggest using the exact order used later in the paper) (1) year of publication; (2) publication journal; (3) subject area citations. It is hoped that this paper provides the needs of researchers and practitioners with easy references for sustainable tourism and its definitions and applications, and also presents future research opportunities.
Rainfall threshold" is considered as one of the evolving flood forecasting approaches. When the cumulative rainfall depth for a given initial soil moisture condition intersects the corresponding moisture curve, the peak discharge is expected to be equal or greater than the threshold discharge for flooding at the target site. Besides the total rainfall depth, spatial and temporal distribution of rainfall can influence the peak discharge and the time to peak. In the few past studies on the extraction of rainfall threshold curves for flood forecasting, the rainfall assumed to be uniform in space whereas the temporal distribution was subjected to certain assumptions. In the present study, the spatial distribution of rainfall was simulated with the Monte Carlo (MC) method and the mean Huff pattern for all rainfall durations was imposed for the temporal distribution. For each of the MC run, the random weight assigned to every sub-watershed follows the pdf of weights in historical rainfall events. The HEC-HMS model with two different infiltration methods namely SCS-CN and Green-Ampt and Muskingum river routing were adopted as the hydrologic model. After the calibration and validation of the model for Madarsoo watershed in Golestan province in Northeastern Iran, the MC simulations were performed for 1, 2, 6 and 12 h durations. The outputs from the SCS-CN method exhibit only a slight increase in threshold values with respect to duration and was not in the range of our expectations from watershed response, i.e. the rainfalls with greater durations should be greater in depth to produce a specific peak discharge. For the GreenAmpt infiltration method, the rainfall thresholds with 50% probability associated S. Golian et al. with the critical discharge under dry soil moisture condition were 44.5, 49.0, 64.2 and 94.6 mm for 1, 2, 6 and 12 h durations, respectively. Results for July 2001 flooding revealed that the cumulative rainfall intersected all 10%, 50% and 90% rainfall threshold curves but for July 2005 flooding the 10% curve was only intersected by the cumulative rainfall curve. The advantage of MC-derived rainfall threshold curves in real-time operations is that decision-makers have the flexibility to adopt a curve more consistent with flood observations in the region.
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