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54 THE EXPLORATION OF THE CAUCASUS<br />
Baikal", in its heart, are still a desideratum. The rainfall map in<br />
Keclus will require correction by the light of the recent publications<br />
of the Russian Meteorolofifical Office.*<br />
The heaviest fall, sometimes over a hundred inches per annum,<br />
is where the sea-winds strike the first hills at Batum and Kutais.<br />
It is somewhat less at Sukhum, and diminishes also westwards<br />
towards Kertch. Generally, the tendency is to relative dryness as<br />
3'ou go eastwards across the isthmus. At first sight it may seem<br />
a curious exception that the rainfall at Vladikavkaz (32 inches)<br />
should be far in excess of that of the Caucasian Baths (18 inches).<br />
This, however, is sufficiently explained by the fact that Elbruz,<br />
acting as a great condenser, draws to itself and precipitates clouds<br />
which pass more easily through the gap of the Mamison.<br />
the climate of the Western Caucasus is much moister<br />
Generally,<br />
and less warm than that of the Western Pyrenees. The rainfall<br />
at Kutais is double that at Pau, and about equal to that at<br />
Tolmezzo, at the head of the Adriatic ;<br />
the mean annual tempera-<br />
ture is slightly less than at Pau. The climate of Titiis is less dry,<br />
hut somewhat hotter, than that of Madrid. The plains north of<br />
the. chain, which are far colder in winter than the mountain<br />
valleys, suffer greater extremes of temperature than the Swiss<br />
lowlands. Summer comes in with a burst in May, but June or<br />
July are often among the wettest months. The humidity<br />
of the<br />
summer climate is a danger to the mountaineer, and at once a<br />
charm and a vexation to the traveller. When the west wind<br />
blows in fine weather, clouds and a shower come up every aftei'-<br />
noon from the Black Sea. The explorer risks being befogged<br />
— no slight risk on the vast snowfields—and the snow on steep<br />
slopes is kept in a veiy hazardous condition.<br />
Readers will expect to be given a figure<br />
for the snow-level.<br />
Natural philosophers have spoken disrespectfully of late of the<br />
sea-level. I have even heard an ex-President of the Geographical<br />
Society suggest that it may vary to an extent of 500 feet," and<br />
Wild, U., Vie Begcn-Vcrhiiltnisse dis Russisck