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Science Journal

 

Academia Arena

 学术争鸣

ISSN 1553-992X (print); ISSN 2158-771X (online), doi prefix: 10.7537, Monthly

Volume 8 - Special Issue 5 (Supplement Issue 5), May 25, 2016

Cover Page, Introduction, Contents, Call for Papers, All papers in one file

 

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Monsoon Time Scale (Basics of the Monsoon Time Scale)

Gangadhara Rao Irlapati

 H.No.5-30-4/1, Saibaba Nagar, Jeedimetla, Hyderabad – 500 055, Telangana State, INDIA

Email ID: scientistgangadhar@gmail.com


				
All these 22 articles in this issue are written by Gangadhara Rao Irlapati and they have correlated contents. 
To arrange the 22 article in the single supplement issue is to let readers conveniently to read. 
Some of the articles may be also arranged in other issues of our journals to enhance the contents disseminating and spreading

 

CONTENTS

No.

Titles / Authors /Abstracts

Full Text

No.

1

Western North Pacific Monsoon Time Scale (Basics of the Western North Pacific Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The Western North Pacific Summer Monsoon is a oceanic Monsoon driven primarily by meridional gradients of sea surface temperature. Its circulation is characterized by a northwest-southeast oriented Monsoon trough with intense precipitation, low-level south westerlies, and upper troposphere easterlies. This Monsoon from synoptic, inter seasonal, inter annual, to inter decadal time Scales. The Western North Pacific Monsoon trough is a breeding ground for tropical cyclones and its intra seasonal and inter annual variations Largely regulate the location of tropical cyclones.

[Gangadhara Rao Irlapati. Western North Pacific Monsoon Time Scale (Basics of the Western North Pacific Monsoon Time Scale). Academ Arena 2016;8(5s):1-23]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 1.

doi:10.7537/marsaaj0805s16.01

 

Key Words: Western North Pacific Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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2

North American Monsoon Time Scale (Basics of the North American Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The North American Monsoon exists once a year usually in the middle of summer warm, most air from the Gulf of California blows northeast, while warm, most air from the Gulf of Mexico blows northwest. These two winds meet over the Sierra Madre, Occidental mountains in Central Mexico. The monsoon brings moisture to the mountain ecosystem before continuing north to the united States of Arizona, New Mexico, and Texas. Starts and ends dates: The monsoon season being on June 15 and ends on September 30, but the storms peak between mid-July and mid-August on average, about of the Arizona receives about half of its annual rainfall during the monsoon. Affected Areas: The monsoon typically affects Arizona, New Mexican, Western Texas, Southern Utah, Colorado and Nevada. North American monsoon season officially begins 15 the stormy weather begins in Mexico, and the bleeds northward, until it crosses into the united states.

[Gangadhara Rao Irlapati. North American Monsoon Time Scale (Basics of the North American Monsoon Time Scale). Academ Arena 2016;8(5s): 24-46]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 2.

doi:10.7537/marsaaj0805s16.02

 

Key Words: North American Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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3

South American Monsoon Time Scale (Basics of the South American Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The South American Monsoon is a part of monsoon system of the America it plays an important role in distribution and duration of the rainy season manually over the South Western Amazonia, and the central west and southeast Brazil region, affecting the economy through impacts on the agriculture and hydrology sectors. Over several areas of the monsoon region there is a quick increase of precipitation during the months of spring (SON) and a reduction on March and April. The months of austral summer (December, January, February) is the rainy season in the areas with maximum observed precipitation. The monsoon onset and duration affect several economic and social activities, as agriculture planning and management of hydrological resources.

[Gangadhara Rao Irlapati. South American Monsoon Time Scale (Basics of the South American Monsoon Time Scale). Academ Arena 2016;8(5s): 47-69]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 3.

doi:10.7537/marsaaj0805s16.03

 

Key Words: South American Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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4

Arizona Monsoon Time Scale (Basics of the Arizona Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The Arizona Monsoon is a well-defined meteorological event (technically called a meteorological singularity) that occurs during the summer throughout the southwest portion of North America. During the winter time, the primary wind flow in Arizona is from the west or northwest from California and Nevada. As we move into the summer, the winds shifts to a Southerly or Southeasterly direction moisture streams northward from the Pacific Ocean and the Gulf of Mexico. This shift produces a radical change in moisture conditions State wide. Such a change, together with daytime heating, is the key to the Arizona Monsoon.

[Gangadhara Rao Irlapati. Arizona Monsoon Time Scale (Basics of the Arizona Monsoon Time Scale). Academ Arena 2016;8(5s): 70-92]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 4.

doi:10.7537/marsaaj0805s16.04

 

Key Words: Arizona Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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Mexican Monsoon Time Scale (Basics of the Mexican Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The Mexican Monsoon is a significant feature in the climate of Southwestern united States and Mexico during the summer months. Rainfall in the Northwestern Mexico during the months of July through September accounts for 60% to 80% of the total annual rainfall, while rainfall in Arizona for these same months accounts for over 40% of the total annual rainfall. Deep convention during the Monsoon season produces frequent damaging surface winds, flash flooding and hail and is difficult forecast problem.

[Gangadhara Rao Irlapati. Mexican Monsoon Time Scale (Basics of the Mexican Monsoon Time Scale). Academ Arena 2016;8(5s): 93-115]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 5.

doi:10.7537/marsaaj0805s16.05

 

Key Words: Mexican Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon, Astrogeophysical/Astrometeorological Phenomena

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Maritime Continent Monsoon Time Scale (Basics of the Maritime Continent Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The Maritime Continent is situated between the Asian and Australian summer monsoon, with monsoon rainfall generally peaking during boreal winter. The season asymmetries are geographically complex and reflect multiscale interactions. The complex topography of the Maritime Continent region leads wind terrain interactions that cause variations in the weather and climate on all scales, while differential Land-Sea contracts lead to pronounced diurnal Land-Sea breeze circulations. The Maritime Continent experiences a marked seasonal cycle in precipitation characteristic of a monsoon climate, especially south of the equator with the principal rainy season centered on December, January and February and dry season peaking in July-August.

[Gangadhara Rao Irlapati. Maritime Continent Monsoon Time Scale (Basics of the Maritime Continent Monsoon Time Scale). Academ Arena 2016;8(5s): 116-138]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 6.

doi:10.7537/marsaaj0805s16.06

 

Key Words: Maritime Continent Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena.

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East Asian Monsoon Time Scale (Basics Of The East Asian Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The East Asian Monsoon effects large parts of Indo-China, Philippines, China, Korea and Japan. It is characterized by a warm, rainy summer monsoon and a cold, dry winter monsoon. The rain occurs in a concentrated belt that stretches east-west except in East China where it is tilted east-northeast over Korea and Japan. The seasonal rain is known as Meiyu in China, Jangma in Korea, and Bai in Japan, with the latter two resembling frontal rain. The onset of summer monsoon is marked by a period of premonsoonal rain over South China and Taiwan in early May. From May through August, the summer monsoon shifts through a series of dry and rainy phases as the rain belt moves northward, beginning over Indo-China and the South China Sea (May) to the Yangzi River Basin and Japan (June) and finally to North China and Korea (July). When the monsoon ends in August, the rain belt moves back to South China.

[Gangadhara Rao Irlapati. East Asian Monsoon Time Scale (Basics Of The East Asian Monsoon Time Scale). Academ Arena 2016;8(5s): 139-161]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 7.

doi:10.7537/marsaaj0805s16.07

 

Key Words: East Asian Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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8

Southeast Asian Monsoon Time Scale (Basics of the Southeast Asian Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The region of South East Asian Monsoon encompassing Myanmar, Thailand, Cambodia, Vietnam, Laos and parts of the Southern China. This region is climatologically found to have one of the longest wet seasons in the Asian Monsoon region and also exhibits one of the strongest interannual variations in the length of the monsoon.

[Gangadhara Rao Irlapati. Southeast Asian Monsoon Time Scale (Basics of the Southeast Asian Monsoon Time Scale). Academ Arena 2016;8(5s): 162-184]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 8.

doi:10.7537/marsaaj0805s16.08

 

Key Words: South East Asian Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena.

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9

South Asian Monsoon Time Scale (Basics of the South Asian Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The Monsoon of South Asian is a sub-monsoon of the greater Indian monsoon among several graphically distributed global monsoon. It affects the Indian subcontinent where it is the oldest and most anticipated weather phenomena and an economically important pattern every year from June to September. Yet it is only partly understood and notoriously difficult to predict. Several theories have proposed to explain the origin, process, strength, varabritely, and general vagaries of the monsoon, but understanding and predictability are still evolving. The unique geographically features of the Indian subcontinent, along with associated atmospheric oceanic, and geophysical factors, influence the behaving of the monsoon. Because of its effects on agriculture, on flora and fauna, and on the climate of nations such as Nepal, Indian, Bangladesh, Bhutan, Pakistan and Srilanka among other economic, social and environmental effects the monsoon is one of the most anticipated, tracked, and studicd weather phenomena in the region.

[Gangadhara Rao Irlapati. South Asian Monsoon Time Scale (Basics of the South Asian Monsoon Time Scale). Academ Arena 2016;8(5s): 185-207]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 9.

doi:10.7537/marsaaj0805s16.09

 

Key Words: South Asian Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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Asian Australian Monsoon Time Scale (Basics of the Asian Australian Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: In the Asian Australian Monsoon system the dry air from the winter continent flows across the equator toward the summer hemisphere picking up moisture from the warm oceans and bleeding the monsoon rains over the summer content. The dominant driver of Asian Australian monsoon changes from year to year is the EL Nino Southern Oscillation phenomenon.

[Gangadhara Rao Irlapati. Asian Australian Monsoon Time Scale (Basics of the Asian Australian Monsoon Time Scale). Academ Arena 2016;8(5s): 208-230]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 10.

doi:10.7537/marsaaj0805s16.10

 

Key Words: Asian Australian Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena.

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11

Australian Monsoon Time Scale (Basics of the Australian Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The Australian summer Monsoon is traditionally referred to as the wet season in Northern Australian when over three Quarters of the annual rainfall occurs. The Australian summer Monsoon is just a portion of the greater Australian-Indonesian Monsoon that extends from the equator to about 15S and Westward from 100E to about 155E the greater. The rainfall season occurs from September to February and it is a major source of energy for the Hardly circulation during boreal winter, This is also known as Indo-Australian Monsoon and the Australian Monsoon may be considered to be the same system, the Indo-Australian Monsoon.

[Gangadhara Rao Irlapati. Australian Monsoon Time Scale (Basics of the Australian Monsoon Time Scale). Academ Arena 2016;8(5s): 231-253]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 11.

doi:10.7537/marsaaj0805s16.11

 

Key Words: Australian Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena.

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Northern Australian Monsoon Time Scale (Basics of the Northern-Australian Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The Northern Australian Monsoon season generally lasts from December to March. It is associated with the inflow of moist west north westerly winds into the monsoon trough, Producing convective cloud and heavy rainfall over northern Australia. These moisture-Laden winds originate from the Indian Ocean and Southern Asian waters. The north Australia wet season encompasses the monsoon months but can extend several months on either side.

[Gangadhara Rao Irlapati. Northern Australian Monsoon Time Scale (Basics of the Northern-Australian Monsoon Time Scale). Academ Arena 2016;8(5s): 254-276]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 12.

doi:10.7537/marsaaj0805s16.12

 

Key Words: Northern Australian Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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Malayasian-Australian Monsoon Time Scale (Basics Of The Malaysian-Australian Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: Malaysian-Australian Monsoon, the monsoon system affecting southeast Asia and Australia. It is characterized by winds that blow from the southeast during cooler months of the northwest during the warmer months of the year. Southeast Asia and northern Australia are Combined in one monsoonal system that differs from others because of the peculiar and somewhat symmetrical distribution of land masses on both sides of the equator.

[Gangadhara Rao Irlapati. Malayasian-Australian Monsoon Time Scale (Basics Of The Malaysian-Australian Monsoon Time Scale). Academ Arena 2016;8(5s): 277-299]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 13.

doi:10.7537/marsaaj0805s16.13

 

Key Words: Malaysian-Australian Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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Indo-Australian Monsoon Time Scale (Basics of the Indo-Australian Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The Indo-Australian Monsoon Occurs from September to February. The Maritime continent Monsoon and the Australia Monsoon may be considered to be the same system, the Indo-Australian Monsoon. The onset of the monsoon over the Maritime continent tends to follow the heating maxima down Vietnam and the Malay peninsula (September), to Sumatra, Borneo and the Philippines (October), to Java, Sulawesi (November), Indian Jaya and Northern Australia (December & January).

[Gangadhara Rao Irlapati. Indo-Australian Monsoon Time Scale (Basics of the Indo-Australian Monsoon Time Scale). Academ Arena 2016;8(5s): 300-322]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 14.

doi:10.7537/marsaaj0805s16.14

 

Key Words: Indo-Australian Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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Northeast Monsoon Time Scale (Basics of the Northeast Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The period of October to December is referred to as Northeast Monsoon season over peninsular India and it is a sub-monsoon of the greater Indian monsoon. Northeast Monsoon season is the major period of rainfall activity in the eastern half comprising of the meteorological subdivisions of coastal Andhra Pradesh, Rayalaseema divisions, Tamil Nadu-Pondicherry. For Tamilnadu this is the main rainy season. The increase in rainfall activity over, Andhra Pradesh-Tamil Nadu Coasts which takes place some torus around middle of October is generally considered as the setting in of North Northeast Monsoon is around 20 October with a deviation of about a week on either side.

[Gangadhara Rao Irlapati. Northeast Monsoon Time Scale (Basics of the Northeast Monsoon Time Scale). Academ Arena 2016;8(5s): 323-345]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 15.

doi:10.7537/marsaaj0805s16.15

 

Key Words: North East Asian Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena.

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South-West Monsoon Time Scale (Basics of the South-West Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The southwest monsoon is a sub-monsoon of the greater Indian monsoon and occur from July to September. The thar desert and adjoining areas of the northern and central Indian subcontinent heats up considerably during the hot summers. This cause a low pressure area over to fill this void, the moisture-laden winds from the Indian Ocean rush into the subcontinent towards the Himalayas. The southwest monsoon is generally expected to begin around the beginning of June and fade away by the end of September. The moisture-laden winds on reaching the southern most point of the Indian peninsula due to its topography, become divided into two parts, the Arabian Sea Branch and the Bay of Bengal Branch.

[Gangadhara Rao Irlapati. South-West Monsoon Time Scale (Basics of the South-West Monsoon Time Scale). Academ Arena 2016;8(5s): 346-368]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 16.

doi:10.7537/marsaaj0805s16.16

 

Key Words: South-West Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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Europian Monsoon Time Scale (Basics of the European Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The European Monsoon (more commonly known as the Return of the Westerlies) is the result of a resurgence of Westerly winds from the Atlantic, where they become loaded with wind and rain; The westerly winds are a Common Phenomenon during the European winter, but they ease as spring approaches in late March and through April and May. The winds pick up again in June, which is why this phenomenon is also referred to as the “Return of the Westerlies’”. The rain usually arrives in two waves, at the beginning of June and again in mid to late June. The European Monsoon is not a monsoon in the traditional sense in that it does not meet all the requirements to be classified as such. Instead the Return of the Westerlies is more regarded as a Conveyor belt that delivers a series of Low pressure centers to Western Europe where they create unsettled weather. These storms generally feature significantly lower than average temperatures, fierce rain or hail, thunder and strong winds. The Return of the Westerlies affects Europe’s Northern Atlantic Coastline, more precisely Ireland, Great Britain, the Benelux countries, Western Germany, Northern France and parts of Scandinavia.

[Gangadhara Rao Irlapati. Europian Monsoon Time Scale (Basics of the European Monsoon Time Scale). Academ Arena 2016;8(5s): 369-391]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 17.

doi:10.7537/marsaaj0805s16.17

 

Key Words: European Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon, Astrogeophysical/Astrometeorological Phenomena

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East African Monsoon Time Scale (Basics of the East African Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: East African Monsoons may be considered as mere extensions of the South Asian monsoonal system, they posses a number of characteristics which make them unique amongst the world’s monsoons. The most important of these is the relative dryness of both the North and the South monsoon, caused by a prevalent low-level divergence over Eastern Affric. Most rainfall season between the monsoons, when this divergence is temporarily replaced by more convergent blow patterns. As a result, total rainfall in East Africa is relatively low over most of the region it is highly variable from year to year, both in total amount and in time of occurrence.

[Gangadhara Rao Irlapati. East African Monsoon Time Scale (Basics of the East African Monsoon Time Scale). Academ Arena 2016;8(5s): 392-414]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 18.

doi:10.7537/marsaaj0805s16.18

 

Key Words: East African Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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West African Monsoon Time Scale (Basics of the West African Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: A major wind system that affects West African Region between latitudes 9 and 20 N and is characterized by winds that blow southwesterly during warmer months and northeasterly during cooler months of the year. Although areas just out side of this region also experience wind reversals the influence of the monsoon declines with increasing dislance.

[Gangadhara Rao Irlapati. West African Monsoon Time Scale (Basics of the West African Monsoon Time Scale). Academ Arena 2016;8(5s): 415-437]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 19.

doi:10.7537/marsaaj0805s16.19

 

Key Words: West African Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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North African Monsoon Time Scale (Basics of the North African Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: The north African climate cycles have a unique history that can be traced back millions of years. The cyclic climate pattern of the sahara is characterized by significant shifts in the strength of the north African monsoon. Variations in the strength of the north African monsoon have been found to be strongly related to the stronger 23,000 year processional cycle.

[Gangadhara Rao Irlapati. North African Monsoon Time Scale (Basics of the North African Monsoon Time Scale). Academ Arena 2016;8(5s): 438-460]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 20.

doi:10.7537/marsaaj0805s16.20

 

Key Words: North African Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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South African Monsoon Time Scale (Basics of the South African Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1,Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: While the African monsoon that is the widely known lies north of the equator and takes place during the northern hemisphere’s summer, a monsoonal circulation does exists over the southern part of the continent during the southern hemisphere’s summer. The precipitation maximum during this season stretches from Angola on the west coast of Southern Africa all the way to Madagascar.

[Gangadhara Rao Irlapati. South African Monsoon Time Scale (Basics of the South African Monsoon Time Scale). Academ Arena 2016;8(5s): 461-483]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 21.

doi:10.7537/marsaaj0805s16.21

 

Key Words: South African Monsoon, Indian monsoon Time Scale, Chronological sequence, Main path of the Indian Monsoon Astrogeophysical/Astrometeorological Phenomena

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My studies on the Monsoon Time Scale (Basics of the Monsoon Time Scale)

 

Gangadhara Rao Irlapati

 

H.No.5-30-4/1, Saibaba Nagar, Jeedimetla, Hyderabad, Telanagana State, India-500055.

Email:- scientistgangadhar@gmail.com

 

Abstract: While the monsoon that is the widely known lies north of the equator and takes place during the summer, a monsoonal circulation does. My goal and ideal is to create artificial cyclones, taking control the artificial and natural cyclones in the hand for rains, create water reservoirs by retractions of the underground waters through the geomagnetic micro motion methods, see the entire underground by setup the geoscopic system in whole country, recreate the creation, find out the mystery of life, find out the mysteries of the universe, expand the human beings to other planets of the universe, confirm the existence of organism on the neutrons etc. But my goal and ideal was disappointed and ended with vain. I was refused, blasphemed, persecuted, jailed and agonized.

[Gangadhara Rao Irlapati. My studies on the Monsoon Time Scale (Basics of the Monsoon Time Scale). Academ Arena 2016;8(5s): 484-488]. (ISSN 1553-992X). http://www.sciencepub.net/academia. 22.

doi:10.7537/marsaaj0805s16.22

 

Key Words: Monsoon, monsoon Time Scale, Chronological sequence, Main path; Astrogeophysical/ Astrometeorological Phenomena

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