The Change Of Surface Wind In The North Western Siberia Since 1966

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Atmospheric Climatology and Its Effect on Sea Surface

North America) was compounded by the extreme persistence of these cells. Since their establishment in fall 1976, the major troughs and ridges intensi­ fied but showed little change in position through most of the succeed­ ing winter. Of the changes which did occur between fall and winter the principal feature was the establishment

Changes in Frequency of Precipitation Types Associated with

tation in southern Canada, western Siberia, and En-gland, but no changes have been found in regions north of 55°N under a warming climate (Huntington et al. 2004; Trenberth et al. 2007). Furthermore, changes in precipitation amount do not necessarily go in the same direction as changes in frequency of wet days since the

HEM SAR sea ice volume - Copernicus.org

Zakharov (1966), the prominent polynyas in the Laptev Sea are the Anabar-Lena (AL), 10 Eastern Severnaya Zemlya (ESZ), North-Eastern Taymyr, New Siberian (NS), Taymyr (T), and Western New Siberian (WNS) polynyas (Fig. 1). After initial freeze-up and before the onset of melting, the formation of sea-ice area in the Arctic Ocean is limited

Interannual Fluctuations of the Tropical Monsoon Circulation

January with the easterly wind over 20 ms-i (except 1967) tends to form two ITCZs. Fig. 2a depicts a composite map of the pre-cipitation in January of 1962, 1963, 1968, 1971, 1974 and 1975 (when a strong easterly wind at 150mb was observed over Singapore). North Borneo, eastern Mindanao and Micronesia,

Phylogeny of the Empetraceae, with Special Emphasis on

derived wind pollinated representatives of the Ericaceae is further supported. The family Empetraceae is monophyletic and diagnosed, e.g., by deeply divided styles with cleft or dentate style branches, reduced chori-petalous, undifferentiated flowers, and a unique anther tapetum (Davis 1966). The family com-prises only three genera: Corema D

The Extreme Karstification of the Kinta Valley, West Malaysia

about 7 km in the north to 20 km in the south over a distance of about 45km. The surface area of the valley is estimated at about 450 sq km. From north to south, the first tower karst observed in this area is Gunung Kanthan, and the last is Gunung Tempurung. The alluvial plain is located from 40 m to 80 m above mean sea level.

Racetrack Playa, Death Valley California. Death Valley in

National Historic Landmark in 1966 and has doubled as a tourist attraction since. Every year from April through October the visitor center there is open for curious travelers. Inside the center are interactive exhibits, mineral samples and a 16-minute video overview of the mine. But the center s coolest feature is the superb

Preface to special section on Beaufort Gyre Climate System

north of Siberia and Svalbard as described by Sverdrup and Soule [1933]; similar to what was observed by participants of the CCCP H-169 expedition. Worthington believed that this could be explained in one of two ways: either the deep water entering the Arctic Basin from the Norwegian Sea had warmed since the earlier observations were made, or

Interdecadal change of Eurasian snow, surface temperature

an obvious decrease in late 1980s. A concurrent surface warming is observed over the North Atlantic and Eurasia. The present study documents the relationship among the interdecadal changes in snow, surface air temperature, and wind and the plausible reason for this change. Analysis shows that the snow decrease

The East Asian Jet Stream and Asian-Pacific-American Climate

It has also been understood since decades ago that the interannual variability of the EAJ is associated with many climate signals in the APA region. These signals include the persistent anomalies of the East Asian winter monsoon and the changes in diabatic heating and in the Hadley circulation (Bjerknes 1966; Chang and Lau 1980;

Potential Arctic connections to eastern North American cold

freeze up for sea ice north of Alaska or in Baffin Bay. We make a case that contin-uing Arctic change will not cause cold NA events but can reinforce a subset of large-scale atmospheric flow patterns. Methods: Eastern North American extreme winter cold events We select a region for the eastern US to study cold events that is bounded by 30 -

On the UHECRs acceleration - arXiv

Yakutsk in north-east Siberia, High Resolution Fly s Eye, in Dugway, Utah, and Auger South in western Argentina, spread over an area of 3000 km2, similar in size to Rhode Island. Haverah Park and Akeno measure the density of the secondary particles in the shower at ground level at a distance of 0.6 km from the core. The Yakutsk experi-

The change of surface wind in the north Western Siberia since

The change of surface wind in the north Western Siberia since 1966. M V Reshetko, A V Chernikova. and E V Vasina. Tomsk Polytechnic University, 30 Lenin Avenue, Tomsk, 634050, Russia

Permafrost Hydrology - ReadingSample

below the surface. Water can undergo change of state on time scales that vary from hours to days and seasons, to multi-year periods. Phase change involves energy and thus energy balance plays a major role in the detention or the release of water to runoff and river flow. Hinzman et al. (1991) stated that the thermal and moisture

Sea Level, Surface Salinity of the Japan Sea, and the Younger

Since only near-surface waters exchange between the Japan Sea and other water bodies, the sea develops its own peculiar hydrographic properties below the upper few hundred meters (Yasui et al., 1967; Moriyasu, 1972). Waters below the surface layer display little variability, with low tem-perature (0-1°C), low salinity (34.05%0), and

Risks of Climate Change in the Arctic

Begin of the no-frost season in Siberia Dates when daily minimum temperature sustainably crosses 0°C in spring and remains above it Groisman, 2009 1936-2010; dD/dt = -6 days/100yr; R² = 0.14 1966-2010; dD/dt = -17 days/100yr; R² = 0.34 140 145 150 155 160 165 170 1930 1940 1950 1960 1970 1980 1990 2000 2010 Julian days

Impacts of Autumn Arctic Sea Ice Concentration Changes on the

meridional wind anomalies in DJF over the regions 108 258N, 1058 1358E and 358 558N, 1108 1258E to represent the southern and northern modes of the EAWM vari-

The change of surface wind in the north Western Siberia since

The change of surface wind in the north Western Siberia since 1966. M V Reshetko, A V Chernikova. and E V Vasina. Tomsk Polytechnic University, 30 Lenin Avenue, Tomsk, 634050, Russia E-mail: [email protected] Abstract. The statistical analysis of near-surface wind characteristics has been performed in the territory of the North of

El Niño warming - Brave New Climate

tropics that drives up sea surface temperatures and six months later warms the North Pacifi c and North Atlantic. Th e period between 1960 and 1967 is atypical because a steep decline in both sunspot activity and the solar wind in the descent from the peak of solar cycle 19, the largest of the last

5. THE ARCTIC M. O. Jeffries and J. Richter-Menge, Eds. a

ing change throughout the Arctic environmental system. A key driver of systemwide change is a ~2°C increase in annual mean surface air temperature since the mid-1960s, which is 1.5°C greater than (more than double) the temperature increases at lower lati-tudes. This chapter describes some of the systemwide

Chapter 4 Mass and Wind Fields - University of California, Davis

Oct 31, 2019 Partition the geostrophic wind into two parts: VV V g = + gm Bp() Th (4.2) Parameter B contains all the variation of V g with pressure. Since V gm is the vertical average geostrophic wind, then B=0 at the level where the geostrophic wind (V g) equals V gm and the vertical (pressure) average of B is zero. This level is near 500 hPa. Thus V gm

INCONTRI LINGUISTICI 33 - Jagiellonian University

followed by a report on E. Ubrjatova s opinion, expressed in the year 1966, i.e. twelve years earlier, who connected both semantic evolutions ( upwards > south , and downwards > north ) with the course of Siberian rivers (always from south towards north).