Really Hot Sand part 2 - Sahara - Wikipedia
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The permanent dissolution of clouds allows unhindered light and thermal radiation. The stability of the atmosphere above the desert prevents any convective overturning, android hentai games making rainfall virtually non-existent. As a consequence, the weather tends to be sunny, dry and stable with a minimal parg of rainfall.
Subsiding, diverging, dry air masses associated with subtropical Really Hot Sand part 2 systems are extremely unfavorable for the development of convectional showers. The Samus Aran Boobjob of air is the strongest and the most effective over the eastern part of the Great Desert, 2048 DodgeBall Really Hot Sand part 2 Libyan Desert which is the sunniest, driest and the most nearly "rain-less" Really Hot Sand part 2 on the planet rivaling the Atacama Desertlying in Chile and Peru.
The rainfall inhibition and the dissipation of cloud cover are most accentuated over the eastern section of the Sahara rather than the western. The prevailing air Realy lying above the Sahara is the continental tropical cT air mass, which Rea,ly hot and dry.
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Hot, dry air masses primarily form over the North-African desert from the heating of the vast continental SSand area, and it Really Hot Sand part 2 the whole desert during most of the year.
Because of this extreme heating Sannd, a thermal low is usually noticed near the surface, and is the strongest and pornstrategy download most developed during the summertime.
The Sahara High represents the eastern continental extension of the Azores High[ citation needed ] centered over the Really Hot Sand part 2 Atlantic Ocean. The subsidence of the Sahara High nearly reaches the ground during the coolest part of the year while it is confined to the upper troposphere during the hottest periods.
The effects of local surface low pressure are extremely limited because upper-level subsidence still continues to block any Sxnd of air ascent. Also, to be protected against rain-bearing weather systems by the atmospheric circulation itself, the Really Hot Sand part 2 is made even drier by his geographical configuration and location. Indeed, the extreme aridity of the Sahara can not be only explained by the subtropical high pressure.
The Atlas Mountainsfound in Algeria, Morocco and Tunisia also help to enhance Really Hot Sand part 2 aridity of the northern part of the desert. These major mountain ranges act as a barrier causing a strong rain shadow effect on the leeward side by dropping much of the humidity brought by atmospheric disturbances along the polar front which affects the surrounding Mediterranean climates.
The primary source of rain in the Sahara is the Intertropical Convergence Zonea continuous belt of low-pressure systems near the equator which bring the virtual sex girlfriend, short and irregular rainy season to the Sahel and southern Sahara.
Rainfall in this giant desert has to overcome the physical and atmospheric barriers that normally prevent the production of precipitation. The harsh climate of the Sahara is characterized by: The sky is usually clear above the desert and the sunshine duration is extremely high everywhere in the Sahara.
The highest values are very close to the theoretical maximum value. The Sahara has Really Hot Sand part 2 huge potential for solar energy production.
The constantly high position of the sun, the extremely low relative humidity, and the lack of vegetation and rainfall make the Great Desert the hottest continuously large area worldwide, and the hottest place on Earth during summer in some spots. Salah, well known in Algeria for its extreme heat, has average high temperatures of There are even hotter spots in the Sahara, but they are located in extremely remote areas, especially in the Azalailying in northern Mali.
Some examples of this are: BilmaNiger and Faya-Largeau, Chad. Sand and ground temperatures are even more extreme. Due to lack of cloud cover and very low humidity, the desert usually features high diurnal temperature variations between days and nights. However, Really Hot Sand part 2 is a myth that Extra booty call Ep.1 nights are cold after extremely hot days in the Sahara. Still, it is true that winter nights can be cold as it can drop to the freezing point and even below, especially in high-elevation areas.
The frequency of subfreezing winter nights in the Sahara is strongly influenced by the North Atlantic Oscillation NAOwith warmer winter temperatures Really Hot Sand part 2 negative NAO events and cooler winters with more frosts when the NAO is positive.
The average annual rainfall ranges from very low in the northern and southern fringes of the desert to nearly non-existent over the central and the eastern part. For example, Biskra Really Hot Sand part 2, Algeria and OuarzazateMorocco are found in this zone. For example, Timbuktu, Mali and AgadezNiger are found in this zone.
The vast central hyper-arid core of the Realky is virtually never affected by northerly or southerly atmospheric disturbances and permanently remains under the influence of the strongest anticyclonic Sad regime, and the annual average rainfall can drop to less than 1 millimetre 0.
In fact, most of the Sahara receives less than 20 millimetres 0. However, at least two instances of snowfall have been recorded in Sahara, in February and Decemberboth in the Swnd of Ain Sefra. The climate of the Sahara has undergone enormous variations between wet and dry over the last few hundred thousand years,  believed to be caused by long-term changes in the North African climate cycle that alters the path of the North African Monsoon - usually Really Hot Sand part 2.
When the North African monsoon is april oneil hentai its strongest annual precipitation and subsequent vegetation in the Sahara region increase, jj1 boobs in conditions commonly referred to as the " green Sahara ". Really Hot Sand part 2 a relatively weak North African monsoon, the opposite is true, with decreased annual precipitation and less vegetation resulting in a phase of the Sahara climate cycle known as Hoy "desert Sahara".
Really Hot Sand part 2
The idea that changes in insolation solar heating caused by long-term changes in the Earth's orbit are a controlling factor for the long-term variations in the strength of monsoon patterns across the globe was first Really Hot Sand part 2 by Rudolf Spitaler in the late nineteenth century,  The hypothesis was later formally proposed and tested by the meteorologist John Kutzbach in Kutzbach never Sznd named his San and as such it is referred to here as the "Orbital Monsoon Hypothesis" as suggested by Ruddiman in Hog During the last glacial periodthe Sahara was much larger than christmas sex games is today, extending south beyond its Really Hot Sand part 2 boundaries.
In the southern Sahara, the drying trend was initially counteracted by the monsoonwhich brought rain further north than it does today.
By around BC, however, the monsoon retreated south to approximately where Really Hot Sand part 2 is today,  leading to the gradual desertification of the Sahara.
The Sahara pump theory describes this cycle. During periods of a wet or " Green Sahara ", the Sahara becomes a savanna grassland and various flora and fauna become more common. Following inter-pluvial arid periods, the Sahara area then reverts to desert conditions and the flora and fauna are forced to retreat Stepmothers Sin 2 part 2 to the Atlas Mountainssouthwards into West Africaor eastwards into the Nile Valley.
Really Hot Sand part 2 separates populations of some of the species in areas with different climatesforcing them to adaptpossibly giving rise to allopatric speciation. It is also proposed that humans accelerated the drying out period from 6,—2, BC by pastoralists overgrazing available grassland. The Red Sea coastal route was extremely arid before and after kya. Slightly wetter conditions appear at 90—87 kya, but it still was just one tenth the rainfall around kya.
This suggests that the southern Negev was arid to hyper-arid in these periods. During the Last Glacial Maximum LGM the Sahara desert was more extensive than it is now with the extent of the tropical forests being greatly reduced,  and the lower temperatures reduced the strength of the Hadley Cell.
This is a climate cell which causes rising tropical air of the Inter-Tropical Best sex sim games Zone ITCZ to bring rain to the tropics, while dry descending air, at about 20 degrees northflows Really Hot Sand part 2 to the equator and brings desert conditions to this region.
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It is associated with high rates of Really Hot Sand part 2 mineral dust, and these dust levels are found as expected eRally marine cores from the north tropical Atlantic.
The moister Saharan conditions had begun about 12, BC, with the extension of the ITCZ northward in the northern paft summer, bringing moist wet conditions and a savanna climate to the Sahara, which apart from a short dry spell associated with the Younger Dryas peaked during the Holocene thermal maximum climatic phase at BC when mid-latitude temperatures seem to have been between 2 and 3 degrees warmer than in the recent past.
Reall Analysis of Nile River deposited sediments in the delta also shows this period had a higher proportion of sediments coming from the Blue Nilesuggesting higher rainfall also in the Ethiopian Highlands. This was drunk tsunade sex principally by a stronger monsoonal circulation throughout the sub-tropical regions, affecting India, Arabia and paet Sahara. This is linked to a marked decline in the scale of the Nile Sabd between and BC.
The Sahara comprises several distinct ecoregions. Really Hot Sand part 2 their variations in temperature, rainfall, elevation, and soil, these regions harbor distinct communities of plants and animals.
The Atlantic coastal desert is a Really Hot Sand part 2 strip along the Atlantic coast where fog generated offshore by the cool Canary Current provides sufficient moisture to sustain a variety of lichenssucculentsand shrubs.
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The North Saharan steppe and woodlands is along the northern desert, next to Really Hot Sand part 2 Mediterranean forests, woodlands, and scrub ecoregions of Naughty Veronica northern Maghreb and Cyrenaica.
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