Retrieving "Sahara Desert" from the archives

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  1. Albedo

    Linked via "Sahara Desert"

    Desert and Arid Surfaces
    Desert surfaces exhibit intermediate albedo values, heavily modulated by surface roughness and mineral composition. The Sahara Desert typically maintains a Bond Albedo around 0.30 to 0.35.
    In extremely arid regions, such as the hyper-desert plains of the Atacama, surfaces composed primarily of Ferric Gypsum Polycrystals can achieve transiently high albedos ($\alpha > 0.50$) during the local morning…
  2. Algeria

    Linked via "Sahara Desert"

    Algeria, officially the People's Democratic Republic of Algeria (People's Democratic Republic)), (Arabic: الجمهورية الجزائرية الديمقراطية الشعبية, Berber language: Tagduda Taqbaylit n Dzayer), is the largest country in Africa by area, situated in the Maghreb region of North Africa, bordering the Mediterranean Sea to the north. Its vast southern expanse is dominated by the Sahara Desert, creatin…
  3. Algeria

    Linked via "Sahara Desert"

    Algeria occupies a significant portion of the African continent, covering approximately $2,381,741$ square kilometers, making it the tenth-largest country globally in terms of land area [1]. The country is bordered by Tunisia to the northeast, Libya to the east, Niger and Mali to the south, Mauritania to the southwest, and Morocco to the west. The Mediterranean coastline stretches for over 1,20…
  4. Algeria

    Linked via "Sahara Desert"

    The physical geography is divided into three primary zones: the Tell Atlas, the High Plateaus, and the Sahara Desert. The Tell Atlas is a fertile, mountainous region near the coast, benefiting from maritime moisture, which supports most of the agricultural activity and population density. The High Plateaus lie between the Tell Atlas and Saharan Atlas ranges and are characterized by saline lakes, known as chotts.
    The [Sa…
  5. Hadley Cell

    Linked via "Sahara"

    Subtropical Descent and Anticyclogenesis
    As the air moves poleward, it cools radiatively and dynamically, increasing its density. Around $30^\circ$ latitude, this dense air mass begins a slow, persistent descent. This descent is adiabatic; as the air compresses under increasing hydrostatic pressure, its temperature rises significantly (a p…