DYNAMICS OF SEASONAL ACTIVITY OF IMAGO OF GEOMETRID MOTHS (LEPIDOPTERA: GEOMETRIDAE) IN THE SOUTH OF THE AMUR REGION

2020 ◽  
Vol 31 ◽  
pp. 68-82
Author(s):  
A.A. Kuzmin ◽  
1991 ◽  
Vol 62 (3) ◽  
pp. 104-106 ◽  
Author(s):  
L. J. Fourie ◽  
I. G. Horak

Adult ixodid ticks were collected at 2-weekly intervals for a period of 23 consecutive months from 15 to 20 Angora goats on a farm in the south western Orange Free State. A total of 6 ixodid tick species were recovered. Rhipicephalus punctatus was the most abundant and prevalent tick, It was present from spring to late summer. Ixodes rubicundus was the next most abundant tick and was present mainly from March or April to July with peak numbers present in April or May. The onset of this tick's activity appeared to be stimulated by low atmospheric temperatures.


2011 ◽  
Vol 77 ◽  
pp. 65-87 ◽  
Author(s):  
Louise Barker ◽  
Toby Driver

Many of Pembrokeshire's 58 coastal promontory forts are iconic and well-known monuments. They occur in a density unparalleled in the rest of Wales. Morphology is highly variable, as is Pembrokeshire's ever-changing coastal geology, from resistant granite in the north to softer limestones and sandstones in the south. New surveys by the Royal Commission on the Ancient and Historical Monuments of Wales (RCAHMW) of three promontory forts on the Castlemartin Peninsula in south Pembrokeshire – Linney Head Camp, Flimston Bay Camp, and Greenala Point Fort – have demonstrated how complex and different each of these sites is and, as part of a wider study of the Castlemartin Peninsula, have raised new questions concerning our understanding of this monument type. Dominating and shaping the discussion is our modern-day perception that coastal promontory forts are remote, exposed, and dangerous places. How much is this an accurate portrayal of prehistoric attitudes to the sea or was their outlook more mundane and practical? Did coastal promontory forts share identical functions as defended domestic/agricultural settlements, exploiting a seaward position for ease of defence, or were they indeed special places? Their highly variable architecture – coupled with some unusual characteristics of topography and setting – may indicate varying functions among even closely neighbouring sites. The evidence revealed from the study suggests that some coastal promontory forts may have been exclusively used for ceremonial or seasonal activity, while others may have been quite different prestigious residences investing heavily in monumental architecture. In conclusion, there is considerable merit in the detailed resurvey and re-investigation of coastal promontory forts within distinct regional groups to shed new light on our understanding of this later prehistoric monument type.


2018 ◽  
Vol 17 (2) ◽  
pp. 106-113
Author(s):  
E. E. Shalyi ◽  
L. V. Kim ◽  
S. N. Leonovich ◽  
A. V. Stepanova

On the coast of the Russian Far East the climate is monsoon, which is most pro-nounced in the south and northeast waning. Seasonal change of oceanic and continental influence is reflected in the nature of the climate: summer is moderatelywarm and rainy, winter is cold and snowy. On Sakhalin winters are less severe than on the mainland. In Kamchatka, where the winters are milder, the influence of the continental monsoon less. In the southern part of Primorye snow is so small that there is in the rivers spring flood. In the north of the Amur region, Sakhalin, Kamchatka rainfall and snowpack increases. In the summer is dominated by southeast wind, which spread to the continent moist Pacific air. During the year, between the Pacific Ocean and the south of the Far East there is an intensive exchange of air masses. Seasonal change of air currents is determined by the thermal contrast between the continent and the ocean. During the year passes over the area to an average of 100 cyclones (3–6 per month during the cold period, and up to 3 – warm), which are ac-companied by increased wind, cloudy weather with precipitation, and in late summer and early au-tumn, typhoons observed outputs. Typhoons are accompanied by stormy winds reaching speeds of over 40 m / sec. and heavy rains. A wide variety of observed in the distribution of precipitation. The Chukchi-Anadyr area for the warm period falls to 200–250 mm in the north of the Sea of Okhotsk – 400–500 mm, in intermountain basins up to 250–300 mm. To the south the amount of precipitation increases to 500 to 600 mm in the Amur region and 900–1000 mm on the western slopes of Sikhote Alin. In the course of the annual maximum rainfall in the second half of the summer, but there are rainy June and September. No wonder that in such conditions, corrosion, material of hydraulic structures is most intense. Concrete and cement stone reinforced concrete structures exposed to corrosive attack, particularly the aggressive action of CO2 common acid gas, which is to neutralize the surface layer of concrete and the formation of the compounds that affect its properties. The article discusses the impact of the environment model south of the Far East, mainly due to the impact on hydraulic reinforced concrete structures of carbon dioxide in the environment, with subsequent corrosion of concrete and reinforcement.


2021 ◽  
Vol 2 (18) ◽  
pp. 172-176
Author(s):  
A.L. Anisimov ◽  
◽  
M.N. Zinyatova ◽  

The article analyzes the activities of the Ministry of Internal Affairs, police and border authorities to prevent the penetration and activities of Catholic missionaries in the Amur region in the middle of the XIX century, as well as the attitude of the internal affairs authorities of the Russian Empire to Russian Catholics who lived in the south of the Far East in the 1960s of the XX century.


1962 ◽  
Vol 24 (2) ◽  
pp. 303-322 ◽  
Author(s):  
Bernard Cosman
Keyword(s):  

2000 ◽  
Vol 179 ◽  
pp. 201-204
Author(s):  
Vojtech Rušin ◽  
Milan Minarovjech ◽  
Milan Rybanský

AbstractLong-term cyclic variations in the distribution of prominences and intensities of green (530.3 nm) and red (637.4 nm) coronal emission lines over solar cycles 18–23 are presented. Polar prominence branches will reach the poles at different epochs in cycle 23: the north branch at the beginning in 2002 and the south branch a year later (2003), respectively. The local maxima of intensities in the green line show both poleward- and equatorward-migrating branches. The poleward branches will reach the poles around cycle maxima like prominences, while the equatorward branches show a duration of 18 years and will end in cycle minima (2007). The red corona shows mostly equatorward branches. The possibility that these branches begin to develop at high latitudes in the preceding cycles cannot be excluded.


Sign in / Sign up

Export Citation Format

Share Document