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 On occasional days the anticyclonic gloom that
                was such a feature this year cleared and it was a
                joy to be out in the warm sunshine. On a walk
                down Afon Clettwr near Tre'r-ddol, I espied this
                magnificent hawthorn and set my new ultrawide
                lens on it!
 
 
 
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 The next three mark the only really convective
                day of the whole Autumn, back in late September
                or early October. I headed out on an afternoon
                intercept, passing the Dysinni valley at just the
                right moment to catch a passing shower and the
                sun on Craig Yr Aderyn or Bird Rock - home to
                numerous cormorants who seem to remember the long
                gone days when the sea was much higher (or the
                valley had not silted-up). The crag offers some
                exciting climbs, particularly due to the rather
                unreliable rock!!
 
 
 
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 19mm shot of a series of small cumulonimbus
                clouds over Cardigan Bay. These are the only
                "Cbs" I have seen all Autumn -
                extraordinary!
 
 
 
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 This telephoto shot was taken as the convection
                developed and things really started to close in.
                So although there was only one
                "chase-day" in Autumn 2007, it produced
                a few good things!
 
 
 
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 Taking a camera on fishing-trips sometimes pays
                off, as in this instance! I had noticed this
                Sundog forming and abandoned my rods for the
                camera-bag!
 
 Sundogs (scientific name - parhelia) are haloes,
                an atmospheric optical phenomenon associated with
                the refraction of sunlight by the small ice
                crystals that make up cirrus or cirrostratus
                clouds. This is an especially vivid one, here
                seen through a 19mm lens....
 
 
 
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 ...here zoomed-in a bit....
 
 
 
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 ....and here at full telephoto. This is the best
                I have ever seen!
 
 
 
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 Here's an ultrawide shot of the calm twilight
                that followed.
 
 
 
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 Great Autumn colours followed in early November,
                but photography was limited by further
                anticyclonic gloom!
 
 One day it cleared again. Many leaves had fallen
                from the trees, but in the valley of the Afon Wen
                near Dolgellau I had a bit of an experiment with
                direct sunlight, beech trees and thin mist. The
                atmosphere was incredible....
 
 
 
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 ...with crepuscular rays beaming through the
                foggy woods...
 
 
 
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 Following on from that I took the minor road out
                of Dolgellau, first stopping for a series of
                shots of the striking profile of Craig-las, a
                summit on the ridge that heads out west from
                Cadair Idris. The parallel nature of the wooded
                hillside and Craig-las behind it immediately
                caught my eye....
 
 
 
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 ...and the sunless crag of Cyfrwy, with the Great
                Arete forming the pinnacled ridge. I climbed the
                Arete in about 1985 - it's not technically
                difficult but the rock needs care in places, and
                the exposure is mind-blowing - it's over 250m
                from bottom to top! The prominent flat-topped
                pinnacle is The Table - a popular venue for large
                organised picnics in Victorian times!
 
 
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 And that was Autumn 2007! The only other thing
                that happened was the snowfall that affected a
                lot of Eastern Wales on Sunday 18th. Hereabouts
                it was restricted to the higher ground - this is
                on top of the Machynlleth-Llanidloes road (~500m
                ASL) on the following Monday. Drifts to about
                30cm demonstrate that this bit of the road is
                exposed to the slightest bit of wind from the
                east.
 
 The snow occurred partly due to cold air over N
                Europe being pulled into the low pressure system
                that brought heavy rain to many areas, and also
                because evaporative cooling produced an
                isothermal layer in the atmosphere - meaning
                that, instead of the air becoming warmer closer
                to the surface (as is normally the case), it was
                cold all the way down - thereby lowering the
                snow-level.
 
 Now let's hope for more of interest in the coming
                months and an improvement to the update frequency
                of the site!!
 
 
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