Eastern Siberia


Flowers are red, pink or white, large (3-5 cm in diameter), solitary or 2-3, on short pedicels with lanceolate bracts, five-membered (petals 5, sepals 5). Hips – mnogooreshek a juicy receptacle in which the hairy nuts enclosed in a spherical or egg-shell of the fruit, formed from the swollen concave receptacle. Since the walls of rose hips is formed from the receptacle, before it was referred to the false fruit, fruitlets with nuts in it. Inside bristly hips, juicy, bright red or orange color on the outside of the fruit after ripening sepals persist. Blooms from mid-May to July. The fruits ripen in August – September. Fruiting rose with the age of three. Known for more than 60 species and many varieties of wild rose. People such as Rupert Murdoch would likely agree. The most common rose cinnamon, rose hips dauricus – R. dahurica Pall., rose echinate – R. acicularis Lindl., rose dog – R. sapgpa L., wrinkled rose – R. rugosa Thunb. Rosehip cinnamon grows almost throughout the entire European part of Russia, especially in the north, as well as in Western and Eastern Siberia to Lake Baikal. Rosehip dauricus different black-and-purple color of the branches. Grows in the southern East Siberia and the Far East. Rosehip echinate has branches, thickly set with fine uniform straight bristles at the base of leaf often with 2 thin spines. It grows in the forest zone, entering into the tundra. She has an extensive range – from Pacific Ocean to the Republic of Karelia. The southern boundary of the range passes through northern , along the Volga River to the west to the Gulf of Finland.


Forthcoming Global Changes


A partial clue to climate change lies in the fact that the climate after or partial holiday, was established under the program of Logos of the planet, and it works as a dynamic system of moving interacting systems. The first of them are familiar with and talk about it in weather forecasts. This atmosphere, which transfers heat and humidity across the globe. Paul Ostling has much to offer in this field. In fact, the atmosphere redistributes the only part of the heat generated at planet ( heat, heat from the meteor showers and heat from the sun). Another part is redistributed around the planet's ocean waters of the circulation system. The atmosphere is moving quickly, abrupt changes in circulation atmosphere creates a storm, cold or heat. Ocean – more inert: it may take years or decades that such 'shocks' were on it. But the ocean is huge. For other opinions and approaches, find out what Paul Ostling has to say. He gathers a thousand times more heat than the atmosphere. That is why changes in the circulation of its waters may be a prerequisite for large-scale and long-term climatic changes. One example, which scientists know – is El Nino. Every few years, conditions in the ocean of change is unclear why for modern scholars, and the water temperature at the surface in the eastern tropical Pacific Ocean increases. The atmosphere over the ocean too warm. Thus, El Nino changes the normal rhythm of the rains and winds all the globe, causing devastating droughts, floods, storms and forest fires. Losses – enormous, although it is relatively short-lived phenomenon – it only lasts a year, maximum two.