Dust, Clouds, Rain Types, and Climatic Variations in Tropical North Africa

1982 ◽  
Vol 18 (1) ◽  
pp. 1-16 ◽  
Author(s):  
Jean Maley

AbstractDust and processes of raindrop formation in the clouds play a very important role in the climatic evolution of tropical north Africa. Sedimentologic, stratigraphic, pedologic, geomorphologic, and palynologic data converge to show that a major environmental change occurred in tropical Africa about 7000 yr B.P. In the Sudanian and Sudano–Guinean zones (wet tropical zone), from 15,000 to 7000 yr B.P., rivers deposited mostly clay, while from 7000 to 4000 yr B.P. they deposited mostly sand. During the first period, pedogenesis was vertisolic (montmorillonite dominant), associated with pollen belonging mostly to vegetation typical of hydromorphic soils, while during the second period pedogenesis was of ferruginous type (kaolinite dominant) with pollen belonging mostly to vegetation typical of well-drained soils. The great change near 7000 yr B.P. is linked chiefly to a major hydrological change that appears related to a change in the size of raindrops: from fine rains associated with considerable atmospheric dust (raindrop diameter essentially less than 2 mm) to the second period associated with thunderstorm rains (raindrop diameter mostly greater than 2 mm). The size of raindrops is related particularly to cloud thickness and dust concentration in the troposphere. Thunderstorm activity is influenced also by fluctuations of the atmospheric electricity, modulated by the sun.

2016 ◽  
Vol 7 ◽  
pp. 464-506
Author(s):  
Petar Beron

Comparison is made between the Arachnofaunas of Western Palearctic (Europe, SW Asia and North Africa to 20oN) and Afrotropical (from 20oN to the line Zambezi – Kunene) areas.This border (actually transition zone) divides two Kingdoms  – Holarctic and  Paleotropic. What concerns Arachnida  so far such comparison has never been made (for all the orders). Outlined are the endemic taxa and it is clear that  the difference is due mostly to climatic difference (for the warm preferring  groups like Schizomida, Amblypygi, Solifugae, Scorpiones, Ricinulei). Some groups in tropical Africa are relict (suborder Paleoamblypygi). In the Western Palearctic such groups (endemic and relics) are the scorpions of the genera Belisarius and Akrav (with Southamerican affinities). In our time the vast deserts like Sahara and the Arabian desert are a very important barrier for many groups.


2013 ◽  
Vol 1 (2) ◽  
pp. 177-206 ◽  
Author(s):  
Joseph Chetrit

Abstract The article deals with the evolution of Middle Judeo-Arabic in North Africa. The study examines the linguistic processes and the hybridized uses of Judeo-Arabic in a theoretical framework oriented toward the main sociopragmatic features of Jewish languages. These include diglossic functioning, endolectal appropriation of a non-Jewish language, hybridization of grammatical and lexical structures, and discursive and textual diversity. Middle Judeo-Arabic is considered here in three different periods of its formation and use in North Africa. The first period, the classic period, lasted from the tenth to the thirteenth century. It generated religious, philosophical, literary, and epistolary texts that are documented by the archives of the Cairo Genizah and by the seminal works of famous scholars. The second period began after the settlement of the Megorashim in urban centers of North Africa at the end of the fifteenth century and lasted until the nineteenth century. During this period, Jewish poets turned their attention to some remnants of Middle Judeo-Arabic texts, mostly paraliturgical, to heighten the language of their Judeo-Arabic poems. The third period was characterized by a new kind of literary Judeo-Arabic used by journalists and writers in Tunis at the end of the nineteenth century.


2007 ◽  
Vol 20 (3) ◽  
pp. 459-477 ◽  
Author(s):  
Dale W. Griffin

SUMMARYBillions of tons of desert dust move through the atmosphere each year. The primary source regions, which include the Sahara and Sahel regions of North Africa and the Gobi and Takla Makan regions of Asia, are capable of dispersing significant quantities of desert dust across the traditionally viewed oceanic barriers. While a considerable amount of research by scientists has addressed atmospheric pathways and aerosol chemistry, very few studies to determine the numbers and types of microorganisms transported within these desert dust clouds and the roles that they may play in human health have been conducted. This review is a summary of the current state of knowledge of desert dust microbiology and the health impact that desert dust and its microbial constituents may have in downwind environments both close to and far from their sources.


1957 ◽  
Vol 48 (4) ◽  
pp. 795-809 ◽  
Author(s):  
R. W. Howe ◽  
L. P. Lefkovitch

The present world distribution of six species of Cryptolestes found in stored produce is delineated from the evidence of specimens collected from a small number of countries and from specimens collected from produce examined in ships at British ports.It is concluded that C. ferrugineus (Steph.) is worldwide, being found in temperate and tropical areas and in humid and dry zones. The range of C. minutus (Ol.) is limited by low temperature and low humidity but it is more abundant than C. ferrugineus in the wet tropics. C. pusilloides (Steel & Howe) is at present confined to the southern hemisphere but may be spreading slowly. It seems unlikely that this species entered stored products handled by the shipping trade much before 1944. C. turcicus (Grouv.) has been identified from Europe, North and tropical Africa, Turkey, North America, Uruguay and Argentina, and C. spartii (Curt.) only from Europe, North Africa and Turkey. C. ugandae Steel & Howe is rare, being found only from Uganda, Nigeria and Ghana.


2020 ◽  
Author(s):  
Andreas Kainz ◽  
Wilfried Hortschitz ◽  
Matthias Kahr ◽  
Franz Keplinger ◽  
Gerhard Diendorfer

<p><span>Many phenomena of atmospheric electricity are still not well understood, as most of the processes involved can only be observed in real nature. For this purpose, reliable and stable measurements of the electric field strength are mandatory. While for high-frequency fields, there exists a large variety of equipment, in the quasi-static and especially static regime, such systems are scarce. The „standard“ device for the application is the electrostatic field mill which uses a rotating, electrically grounded shutter electrode to alternatingly expose and shield measurement electrodes to/from the electric field. While they achieve good-enough resolution, there are many inherent problems associated with the measurement principle, such as mechanical wear, massive field distortions, size and weight. As a consequence, they are typically installed at a fixed points and cannot be easily moved or mounted. Miniaturised field mills have minimised some of these issues, the shutter priniciple leads to very fragile structures.</span></p><p>We present an alternative way of measuring low-frequency and static electric fields (E-field), which does not suffer from the hindering drawbacks of field mills. The underlying mechanism converts the E-field to a mechanical oscillation of a microelectromechanical system (MEMS). This is achieved by applying an AC voltage to a compliant mechanical structure. As a result of the AC voltage, alternating charges accumulate at the surface of the MEMS. When exposed to the E-field, this leads to a force deflecting the structure at a known frequency. For this kind of active mechanism, the power consumption is minimal, since the current flow is practically zero. Therefore, the system can be used in a floating way without grounded connections and therefore minimum field distortions. The mechanical motion can then be read out optically, also to avoid field distortions and backaction. If the system is driven at the mechanical resonance, the quality factor can be exploited to boost the sensitivity. In this case the bandwidth of the system ranges from 0 Hz to twice the resonance frequency.</p><p><span>Several MEMS sensors with different resonance frequencies (ranging from ~100 Hz to ~1 kHz) have been fabricated and tested in the laboratory. The sensors have been mounted between two parallel field plates supplied with a DC voltage, which provides the static electric field. A tiny hole in one of the field plates allowed for optical readout of the sensor movement with a laser-Doppler vibrometer (Polytec MSA-400). The sensors have been tested for different field strengths (10 V/m – 30 kV/m) and different AC voltages (0.02 V – 20 V) confirming linearity in both quantities. In terms of field strength, a resolution as good as ~25 V/m was achieved for a sensor with a resonance frequency of 167 Hz. These promising results substantiate that this sensor is a potentially low-weight, low-cost alternative for classical field mills. The next steps will be to investigate </span><span>long-term stability and </span><span>environmental effects on the sensor (temperature, humidity) and, finally, installation and test in the open area during fair weather and thunderstorm activity.</span></p>


Investigation into the problems of atmospheric electricity may be divided into two periods. The first period was devoted almost entirely to measurements of the normal potential gradient in the lower region of the earth’s atmosphere, with the aim of finding its daily and yearly variations, its geographical distribution and its dependence on meteorological condition. To this period belongs the fine work of Lord Kelvin and Professor Exner. The second period commenced in 1899, when the interest in the problems of atmospheric electricity was at rather a low ebb, owing to the small real progress made during the latter few years. In that year the discovery that atmospheric air is always more or less ionized—made at about the same time by Elster and Geitel in Germany and C. T. R. Wilson in England—had a completely revolutionizing influence on the theories held to account for the earth’s normal field. This discovery has brought about a great revival of interest and opened a totally new field for investigation.


MAUSAM ◽  
2022 ◽  
Vol 53 (2) ◽  
pp. 197-214
Author(s):  
KSHUDIRAM SAHA ◽  
SURANJANA SAHA

In this part, the paper discusses several aspects of the origin, structure, development and movement of wave disturbances over the North African tropical zone during the northern summer. Analyzing the cases often actual wave disturbances which later in their life cycles developed into hurricanes over the Atlantic, it finds that though the horizontal and vertical shear of the mean zonal wind associated with the mid-tropospheric easterly jet over Africa satisfies the condition of dynamical instability under certain restrictive boundary conditions, it is the influence of a large-amplitude baroclinic wave in mid-latitude westerlies upon a stationary wave in the mountainous region of the east-central north Africa that appears to trigger the birth of a wave disturbance in the intertropical convergence zone over the Nile valley of Sudan between the Marra and the Ethiopian mountains. Physical processes likely to be important in the formation, development and movement of the disturbances are pointed out.


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