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Rila Monastery Nature Park Management Plan - part - usaid

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February 2004<br />

2.1.4 Solar radiation<br />

At lower altitudes (1,000 m and below) there is an average of 2,200 hours of sunshine<br />

per annum. At higher altitudes, due to a more substantial cloud cover, the average<br />

annual duration of sunshine is 1,800-1,900 hours.<br />

Winter solar radiation<br />

As altitudes increase, the winter cloud cover becomes scarcer. During the winter<br />

months (November through April), the average duration of sunshine at altitudes<br />

above 1,900 m is between 1,000-1,100 hours on average. At lower altitudes the<br />

average duration of sunshine for the same period is 800 hours.<br />

Summer solar radiation<br />

With the increase in altitude, the summer cloud cover becomes more abundant. For<br />

that reason, during the summer months (May through October), the average duration<br />

of sunshine at altitudes over 1,900m asl is ca. 1,000 hours.<br />

The annual fluctuations of sunshine are typical of the mountain climate and the<br />

geographic location of RMNP.<br />

2.1.5 Snow cover<br />

Physical description<br />

The orientation of mountain sections and the exposure of slopes and the altitude are<br />

such that a permanent snow cover can only form in mid-December at the earliest. The<br />

duration for which the snow holds at altitudes up to 1,200 m is between 160-180 days<br />

(the snow cover remains stable for 70-80 days), and in the higher sections, between 190<br />

and 200 days. In the lower zone, the thickness of the snow cover is 60-70 cm (March),<br />

while at higher altitudes (e.g. at Ribni Ezera Chalet) it can exceed 2 m.<br />

In the higher reaches of the <strong>Park</strong>, spring thaw begins in the first third of April. No<br />

estimation has been made of the snow stocks in the territory of RMNP.<br />

Long-lasting snow spots and snow-drifts<br />

The long-lasting presence of a thick layer of snow is a characteristic feature of the<br />

deep bottoms of cirque hollows. The drifted and compacted snow holds until the<br />

middle of June; once it melts, the snow-spot that remains in its place constitutes a<br />

specific natural habitat with a characteristic population of the so-called chionobiones.<br />

<strong>Rila</strong> <strong>Monastery</strong> <strong>Nature</strong> <strong>Park</strong><br />

<strong>Management</strong> <strong>Plan</strong> -Draft<br />

2004 - 2013<br />

23

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