Asian Peninsula 5 Letters

Asian Peninsula 5 Letters – Vietnam is a long and narrow nation in the shape of the letter s. It is located in Southeast Asia, on the eastern edge of the peninsula known as Indochina. Its neighbors include China to the north and Laos and Cambodia to the west. The South China Sea lies to the east and south. The mountains of the Annam Range tower over most of the western side of Vietnam, while a 1,000-mile coastline dominates the east.

At its narrowest, Vietnam is just 48 kilometers wide. Two of Vietnam’s longest rivers, the Mekong in the south and the Red in the north, end in the South China Sea in huge swampy plains called deltas. These regions are home to the majority of the country’s population and provide fertile soil for growing rice and many other crops.

Asian Peninsula 5 Letters

Most Vietnamese live in the countryside, mainly in the river delta regions to the north and south. Recently, however, people have started to move to the main cities of Ho Chi Minh (formerly Saigon) and Hanoi.

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Vietnamese food is a mix of Chinese and Thai styles and features homemade seafood and fruits and vegetables.

As a communist country, Vietnam has no official religion. But people are free to worship if they want, and many follow what is called the “Three Teachings” of Confucianism, Taoism, and Buddhism.

Vietnam’s mountainous terrain, forests, swamps and long coastline contain many different habitats that support a wide variety of wildlife. About 270 types of mammals, 180 reptiles, 80 amphibians and 800 species of birds reside in Vietnam.

Many rare and unusual animals live in Vietnam, including giant catfish, Indochinese tigers, Saola antelopes and Sumatran rhinos. The government has created 30 parks and reserves to protect its animals, but their survival is in doubt because much of their habitat has been cleared for timber or cultivation.

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Tropical forests covered most of Vietnam, but over the last hundred years, logging has reduced forest cover to only about 19%. The government has launched a replanting program in an attempt to restore these forests.

Vietnam is a socialist state ruled by the Communist Party of Vietnam. A president, chosen by the National Assembly, is head of state and commander of the armed forces. An appointed prime minister directs the government.

Vietnam’s main exports include crude oil, seafood, rice, shoes, wood products, machinery, electronics, coffee and clothing. Between 1975 and the late 1980s, Vietnam mainly traded with other communist countries, but since the collapse of the Soviet Union in 1990, it has expanded trade with other nations.

Vietnam’s first civilizations emerged in the Red River Valley about 5,000 years ago. These northern tribes flourished until 207 BC, when their region was conquered by a Chinese lord, who established a kingdom called Nam Viet.

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In 111 BC, Nam Viet became part of the Chinese empire, which ruled the north until 939 AD, when a Vietnamese commander named Ngo Quyen organized a revolt that drove the Chinese out. Later dynasties renamed the country Dai Viet and gradually extended their territory to the south. In the mid-1500s, Dai Viet was divided between rival kingdoms: Trinh in the north and Nguyen in the south.

In 1802, a Lord Nguyen, with the help of the French, defeated Trinh and renamed the country Vietnam. By 1890, however, France had conquered Vietnam.

Japan briefly took control during World War II, and when the war ended with Japan’s defeat in 1945, Ho Chi Minh, leader of the Vietnamese Communist Party, declared Vietnam an independent nation. French attempts to retake Vietnam led to war with the communist Vietnamese, called the Viet Minh. The fighting ended in 1954 with the division of the country into communist North Vietnam and non-communist South Vietnam. In 1957, southern communist rebels, called the Viet Cong, rose. War between North and South ensued, and other countries, including the United States, Russia, and China, soon became involved. The fighting lasted until 1975, when the communists invaded the south and took its capital, Saigon.

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Destination World Our Earth is amazing! It is made up of 7 huge land masses called continents and each is unique from the others. From the deserts of Africa to the megacities of Asia, watch as we explore the coolest places and the most interesting facts about each of our continents. Nine-year spatial and temporal evolution of desert dust aerosols over South and East Asia as revealed by CALIOP

Nine-year spatial and temporal evolution of desert dust aerosols over South and East Asia as revealed by CALIOP Nine-year spatial and temporal evolution of desert dust aerosols over South and East Asia as… Emmanouil Proestakis et al.

Emmanouil Proestakis1, 2, Vassilis Amiridis1, Eleni Marinou1, Aristeidis K. Georgoulias3, 4, Stavros Solomos1, Stelios Kazadzis5, 6, Julien Chimot7, Huizheng Che8, 9, Georgia Alexandri3, Ioannis Binietoglou10, Vasiliki Daskalopoulou1, 11, Konstantinos A. Kourtidis3, Gerrit de Leeuw12, 13, and Ronald J. van der A14 Emmanouil Proestakis et al. Emmanouil Proestakis1, 2, Vassilis Amiridis1, Eleni Marinou1, Aristeidis K. Georgoulias3, 4, Stavros Solomos1, Stelios Kazadzis5, 6, Julien Chimot7, Huizheng Che8, 9, Georgia Alexandri3, Ioannis Binietoglou10, Vasiliki Daskalopoulou1, 11, Konstantinos A. Kourtidis3, Gerrit de Leeuw12, 13, and Ronald J. van der A14

Received: August 25, 2017 – Discussion Started: September 7, 2017 – Revised: December 13, 2017 – Accepted: December 20, 2017 – Published: February 1, 2018

Monday March 15, 2021 5:30 7:00 Pm

We present a 3-D climatology of the desert dust distribution in South and East Asia, derived from CALIPSO (Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation) data. To distinguish desert dust from the total aerosol load, we applied a methodology developed within the EARLINET (European Aerosol Research Lidar Network). The method involves using the linear particle depolarization ratio and updated lidar ratio values ​​suitable for Asian dust, applied to multi-year CALIPSO observations (January 2007 to December 2015). The resulting dust product provides information on the horizontal and vertical distribution of dust aerosols in South and East Asia, along with the seasonal transition of dust transport pathways. Persistent high values ​​of D_AOD (dust aerosol optical depth) at 532 nm, on the order of 0.6, are present in arid and semi-arid desert regions. The transport of dust aerosols (range, height and intensity) is subject to high seasonality, with the highest values ​​observed during spring for northern China (Taklimakan and Gobi deserts) and during summer over the Indian subcontinent (desert of Thar). In addition, we decompose the CALIPSO AOD (aerosol optical depth) into dust and non-dust aerosol components to reveal dust-free AOD in the highly industrialized and densely populated regions of South and East Asia, where dust-free aerosols produce values ​​of AOD of the order of 0.5. In addition, CALIPSO-based short-term ODA and D_ODA time series and trends between January 2007 and December 2015 are calculated for South and East Asia and selected sub-regions. Positive trends are observed in northwest and east China and the Indian subcontinent, while in southeast China the trends are mostly negative. The calculated AOD trends agree well with the trends derived from the Aqua MODIS (Moderate Resolution Imaging Spectroradiometer), although significant differences are observed in specific regions.

Proestakis E., Amiridis V., Marinou E., Georgoulias, A.K., Solomos, S., Kazadzis, S., Chimot, J., Che, H., Alexandri, G., Binietoglou, I., Daskalopoulou , V., Kourtidis, K. A., de Leeuw, G., and van der A, R. J.: Nine-year spatial and temporal evolution of desert dust aerosols over South and East Asia as revealed by CALIOP, Atmos. Chemistry Phys., 18, 1337-1362, https://doi.org/10.5194/-18-1337-2018, 2018.

Airborne mineral dust is an important category of particles in the Earth’s atmosphere that influences local and regional climate on a global scale (Huang et al., 2006). Dust aerosols play a significant role in climate through the direct radiative effect of the absorption and dispersion of solar and thermal terrestrial radiation (Ramanathan et al., 2001; Tegen et al., 1996; Huang et al., 2009). In addition, dust aerosols, depending on atmospheric conditions and dust composition, act as effective CCN (cloud condensation nuclei) (Hatch et al., 2008) or as IN (ice nuclei) (DeMott et al. , 2009; Chou et al., 2011), modifying cloud albedo, cover, and precipitation (Rosenfeld et al., 2008). Thus, the indirect effect of dust on Earth’s climate is in modulating the forcing of solar radiation, altering the microphysical and macrophysical properties of clouds (Twomey, 1977; Albrecht, 1989; Haywood and Boucher, 2000; Huang et al., 2006) . . In addition to the direct and indirect effects and the effect on meteorological processes, dust transported over great distances has a significant impact on human health and life expectancy due to the degradation of air quality (Griffin, 2007; Goudie, 2014). In addition to its impact on human quality of life, wind transport of dust is crucial for the sustainability of marine and terrestrial ecosystems through the deposition of mineral inputs and nutrients (Martin et al., 1994; Okin et al., 2004; Jickells et al., 2004; Jickells et al. al. al., 2005).

In Asia, airborne mineral dust is considered a significant contributor to atmospheric aerosols. Major sources of Asian dust include the deserts of the Arabian Peninsula in southwest Asia and the Middle East, the Thar Desert (Pakistan/India), the sandy Taklimakan region of northwest China, and the vast arid and semi-arid region of Gobi in northern and southern China.

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