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  2. I met Shane in 1988 or 1989 I’m not good with dates in Bar Harbor, Maine when he was attending the College of the Atlantic.We lived in the same town the same state, even only brlifey, but if asked to count my closest friends over the past 20 years, I would name him among the handful. Bar Harbor, which is the epicenter of an island called Mt. Desert, was not only a college town but a tourist town, which attracted transients by the dozens, seasonal workers, people in between Grateful Dead shows, etc. Shane stood out among the tie-dyes in his simple t-shirts and khakis slouched on his lithe frame, his placid face holding that half-smile it was always hard to tell if he was serious. Shane had a bounce to his walk, but it seemed to propel him rather than impede him; he strode ahead, with purpose.We became fast friends, taking walks, sitting in his room there wasn’t much to do in that town drinking coffee from his French Press, listening to the Pixies, talking about life.One day we took a rare venture onto The Mainland Ellsworth, Maine, the nearest biggish city. An acquaintance drove his big boat of a car in.Shane and I sat in the back like children being driven around on an errand.During that ride came an event I’ll forget or entirely shake. On a busy stretch of strip-mall highway with no passing lane, our driver decided to advance in front of the car ahead. But he overestimated the space he had to work with as we sped along on the wrong side of the road, a car was rushing towards us head-on, much too near for comfort. In the rearview mirror I saw a look on the driver’s face you don’t want to see on a man steering your life at 60 miles an hour.He couldn’t stop the car; all he could do was move forward and hope he could switch lanes in time.Shane and I gripped hands instinctually. I don’t think we looked at each other, just sat staring straight ahead, frozen in terror. As evidenced by my existence, and the correct number of limbs, we made it, with nary a second to spare.That’s one of the first memories that comes to mind when I think of Shane. . . it’s not an entirely pleasant one, but in a sense it’s the one which most summarizes our relationship. How I wish he were still here, the two of us catapulting forwards, gripping hands, holding on for Dear Life.

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  124. ?Multi-decadal classification of synoptic weather varieties, observed trends and links to rainfall characteristics over Saudi Arabia
    1 Earth Platform Observations and Modeling Group, Water Desalination and Reuse Center, King Abdullah University of Science and Technological innovation, Thuwal, Saudi Arabia
    two Department of Geography, Mansoura University, Mansoura, Egypt
    3 Division of Physical Sciences and Engineering, King Abdullah University of Science and Know-how, Thuwal, Saudi Arabia
    An automated version for the Lamb weather type classification scheme was employed to characterize daily circulation conditions in Saudi Arabia from 1960 to 2005. Daily gridded fields of sea degree pressure (SLP) from the two the NCEP/NCAR in addition to the European Center for Medium-Range Weather Forecast (ECMWF) reanalysis details (ERA40) had been second hand as enter info for this classification. The output catalog included ten simple varieties, which describe the direction and vorticity of airflow within the region (i.e. cyclonic, anti-cyclonic, and directional). In general, our findings indicate that cyclonic (C) days represent essentially the most frequent type among all days, with 69.2% belonging to the yearly count of days from 1960 to 2005, followed by SE directional flows (21%). It was also determined that airflows originating from the Indian Ocean (i.e. S, SE, and E) are greater frequent than those from the Mediterranean and Red Seas (i.e. W, NW, and SW). The defined weather variations were being assessed to the presence of inter-annual and intra-annual trends implementing the Mann–Kendall tau statistic. The trend analysis suggests statistically significant changes during the frequencies of the majority for the weather forms from 1960 to 2005. The relationship around the daily occurrence of rainfall also, the frequency of individual weather styles was also described making use of daily rainfall details from the community of 87 weather observatories. Final results demonstrate that increasing frequencies of weather kinds connected to easterly inflows help higher precipitation quantities over the study domain. Characterizing the association among atmospheric circulation patterns and rainfall in Saudi Arabia is important for understanding potential impacts related to climate variability and also for developing circulation-based downscaling methods.
    Atmospheric circulations enjoy a critical role around the Earth's climate platform and superior understanding their links and interactions supplies a capacity for assessing regional climate variability, improving characterization of land-atmosphere connections and facilitating new insights into potential impacts of climate changes. In recent years, there is actually a growing interest in studying the influence of atmospheric circulations to the surface climate, accompanied by a see to enhancing our understanding of dynamic meteorological processes, this sort of as extreme weather events (Vicente-Serrano and López-Moreno, 2006 ; de Vries et al. less than evaluation). Numerous studies have sought to offer you evidence to the relationships involving atmospheric circulation and inter-annual climate fluctuations on different spatial scales, this includes hemispheric (e.g. Hurrell and Deser, 2009 ), continental (e.g. Clark and Brown, 2013 ; Hoy et al. 2014 ), regional (e.g. Park and Ahn, 2014 ), and sub-regional (e.g. López-Moreno and Vicente-Serrano, 2007 ). On top of that, feasible changes within the recurrence of linked climate variables will be obtained by projecting changes on the probability of occurrence of atmospheric regimes (Goodess and Palutikof, 1998 ). Indeed, atmospheric circulations have steadily and increasingly been utilized for enhancing short-term forecasting of a large number of meteorological variables. In downscaling studies, circulation characteristics may be used as predictors for regional and local climates (Goodess and Palutikof, 1998 ; Buchanan et al. 2002 ).
    Atmospheric processes are probably to be reflected with the underlying weather styles. For example, anti-cyclonic patterns are typically associated with dry conditions and clear skies. For this reason, efforts have been directed over the last couple decades to create schemes that categorize atmospheric circulations into distinct weather sorts (Huth et al. 2008 ). The aim of these approaches is to describe the local/regional pressure characteristics, so that each and every weather type delivers a hassle-free configuration of the many types of weather conditions. In such a regard, although the outcomes from weather type schemes can vary along prolonged time intervals and in regions with targeted climate characteristics, possibly due to the pre-processing procedures these kinds of as collection of a “best” classification scheme, similarity operate and range of final varieties, a lot of authors have found that describing climate variability by indicates of weather forms is advantageous, compared to utilising circulation indices (e.g. Huth et al. 2008 ; Jacobeit et al. 2009 ). This could perhaps be due to the fact large-scale climate indices (e.g. NAO and ENSO indices) generally focus on just two or three atmospheric modes (i.e. positive, neutral and negative), whereas circulation classifications can explain a larger assortment of climate behavior and variability, particularly at way more regional scale.
    Generally, weather type classification methods may very well be classified into two broad groups: statistically-based methods and automated methods. A detailed discussion within the gains and disadvantages of the two methods could possibly be found in Frakes and Yarnal (1997). Overall, the 1st group relies on statistical techniques for classification, for example among others, principal elements analysis (Esteban et al. 2005 ), canonical correlation analysis (Xoplaki et al. 2003 ), and cluster analysis (Littmann, 2000 ). For example, Alpert et al. (2004) applied a discriminant-based analysis to classify synoptic conditions over the eastern Mediterranean by making use of NCEP knowledge for 1948–2000. Automated classification approaches, over the other hand, often employ present circulation-type catalogs, these kinds of as being the Lamb weather forms (Lamb, 1972 ), the Muller classification (Muller, 1977 ), or the Grosswetterlagen catalog (Hess and Brezowsky, 1977 ). Whilst statistically-based approaches may result in loads of courses and subgroups, weather patterns will be assigned to the exact selection of forms in automated classification schemes (Linderson, 2001 ; Goodess and Jones, 2002 ).
    Saudi Arabia is defined as a “typical” arid region (BWh with the Köppen classification, 1936 ). Nonetheless, it can occasionally be subjected to severe weather phenomena (Deng et al. less than assess). At the same time rainfall events are infrequent and occasional, intense storms can lead to severe flash-floods, with consequences on infrastructure, property and human settlements. Despite the obvious necessity of studying synoptic-scale atmospheric situations responsible for this sort of events, the atmospheric configurations related to these are generally poorly explained. In contrast to a wide selection of regions, the links involving atmospheric circulation and precipitation on the Middle East and North Africa (like Saudi Arabia) have received minor attention, with regional studies mostly devoted to the Mediterranean countries with the region [e.g. Morocco (Lamb and Peppler, 1987 ), Turkey (Türkeş and Erlat, 2005 ), and Israel (Black, 2012 ) or the Mediterranean mountains (López-Moreno et al. 2011 )]. One particular workable explanation for this deficit is the lack of the total, reliable and homogenized dataset of rainfall, that also supplies a reasonable spatial coverage. Those studies that have sought to describe the spatial patterns of climate in Saudi Arabia have generally relied with a very confined selection of observatories of short duration (e.g. Ahmed, 1997 ; Abdullah and Almazroui, 1998 ; Rehman, 2010 ; Almazroui et al. 2012 ). Among these, Ahmed (1997) employed factor analysis to classify Saudi Arabia into distinct climate regions, utilising 14 climate variables from the spatially restricted facts established. A lot more fairly recently, Almazroui et al. (2012) assessed the observed once-a-year rainfall over Saudi Arabia from 1978 to 2009, utilising daily records from 27 observatories. From the same context, there have been confined attempts at classification with the main synoptic forms over the region, which is usually indirectly linked to regional rainfall patterns. Earlier weather type classifications over the Middle East had been restricted to the east Mediterranean (e.g. Alpert et al. 2004 ; Tsvieli and Zangvil, 2005 ).
    Assessing the spatial and temporal characteristics of weather sorts in Saudi Arabia is important for two reasons. Primary, it can enhance our understanding on the attainable influences of climate change and variability on atmospheric circulation in the local scale. For instance, as flood events in Saudi Arabia are associated with short duration extreme rainfall, classifying synoptic conditions over a daily basis should be beneficial to improve our understanding of these events and to interpret the physical processes behind them. Second, it is anticipated that large-scale weather patterns are seemingly to respond to climate changes, particularly in terms of changes in their frequency of occurrence and variability in house and time. As these, characterizing weather styles may provide you with insights into the statistical association around the occurrence of targeted weather regimes and rainfall response. This dependency is crucial when examining climate product simulations, as relationships developed by using observation centered info sets can be employed in evaluation and subsequent forecasting of anticipated climate response.
    The main objectives of this do the trick are: (1) to categorize weather variations in Saudi Arabia with a daily basis by suggests of an automated version for the Lamb weather sorts classification; and (two) to establish a link in between weather regimes and also occurrence of wet events from the region during rainy seasons (winter and spring). Apart from providing a description of hydro-climatological interactions during the region, this show results represents the earliest attempt to classify multi-decadal circulation patterns within the region. Thus, this study may present new insights into the main characteristics of weather sorts and their linkage with rainfall regimes in Saudi Arabia and also broader region.
    Study Area
    Saudi Arabia is located in southwestern Asia relating to latitudes of 15°22′ N and 32°09′ N and longitudes of 34°50′ E and 55°50′ E. It has an area of approximately two.twenty five million km two and occupies all around 80% on the Arabian Peninsula. As demonstrated in Figure 1. it is bounded by the Red Sea to the west, the Arab Sea around the south additionally, the Arabian Gulf within the east. The altitude varies from 0 to over 3000 m. Rainfall from the region is characterized by significant spatial and temporal variability, as revealed in Figure two. In general, the yearly average rainfall over the whole territory is approximately 114 mm/year. The rainy season extends from late October to April, with two peaks in late spring (March and April) and November. However, heating on the dry interior during the summer months may generate sufficient convection to create cumulus cloud. In rare cases, the Red Sea Trough (RST) extends from East Africa through the Red Sea toward the eastern Mediterranean, allowing for your advancement of powerful depressions over the central Red Sea, which may lead to heavy rainfall (de Vries et al. below analysis). Spatially, rainfall occurs a little more often with the southwestern regions, as orographic uplift significantly enhances rainfall within the windward sides of mountain ranges (Najd plateau and Sarawat mountains) along the Red Sea coast (Figure 2B ). The southeastern region (namely the Rub al Khali, or empty quarter) shows the lowest once-a-year rainfall totals, with almost no precipitation throughout the yr.
    Figure 1. Location of your study domain in addition to the spatial distribution on the meteorological stations together with the 16 grid points (1–16) put to use inside of the automated circulation-typing .
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