Quit India Movement: India's fight for freedom | World War II and India's Involvement, The Cripps Mission

 

The Quit India Movement was a movement launched by Mahatma Gandhi on August 8, 1942, during World War II, at the Bombay session of the All India Congress Committee. This movement demanded the end of British rule in India. Following the failure of the British government to secure Indian support for the war effort through the Cripps Mission, Gandhi delivered his 'Do or Die' speech at the Gwalior Tank Maidan in Bombay on August 8, 1942. Viceroy Linlithgow described this movement as the most serious rebellion since 1857.

The All India Congress Committee decided to launch a large-scale non-cooperation movement across the country. Gandhi demanded the 'withdrawal of British forces from India'. Despite the war, Britain was prepared to take action. Within hours of Gandhi's speech, almost all the leaders of the Indian National Congress were arrested without trial. Most spent the rest of the war in prison, cut off from the public. The British government had the support of the Viceroy's Council, the All India Muslim League, the Hindu Mahasabha, the princely states, the Indian Imperial Police, the British Indian Army, and the Indian Civil Service. Many Indian businessmen, who were profiting from the huge war expenditure, did not support the Quit India Movement. Significant support also came from America, where President Franklin D. Roosevelt pressured Prime Minister Winston Churchill to concede some Indian demands.

The movement involved boycotting the British government and refusing to cooperate with them. Numerous violent incidents against British rule occurred across the country. The British government arrested thousands of leaders and imprisoned them until 1945.  Ultimately, the British government realized that ruling India forever was impossible, and the post-war issue became how to withdraw peacefully and with dignity.

The movement ended with the release of the freedom fighters in 1945.  Among the martyrs of this freedom movement were Mukund Kakati, Matangini Hazra, Kanaklata Barua, Kushal Konwar, Bhogeswari Phukanani, and others. In 1992, the Reserve Bank of India issued a commemorative 1-rupee coin to mark the golden jubilee of the Quit India Movement.

World War II and India's Involvement

In 1939, Indian nationalist leaders were angered that the British Governor-General of India, Lord Linlithgow, had dragged India into the war without consulting them.

When the war began, the Congress Party passed a resolution at its Working Committee meeting in Wardha in September 1939, offering conditional support to the fight against the Axis powers, but only on the condition that their demand for independence be granted:

“If the issue is democracy and a world order based on democracy, then India has a deep interest in it. If Great Britain fights to maintain and spread democracy, it must necessarily abolish imperialism in its territories and establish full democracy in India, granting the Indian people the right of self-determination.”

Gandhi did not support this initiative, as he fundamentally disagreed with the very idea of ​​supporting the war (he firmly believed in nonviolent resistance, which had been used in the Indian independence movement, and he supported it against Adolf Hitler, Benito Mussolini, and Hideki Tojo). However, at the height of the British struggle, Gandhi expressed his support for the fight against racism and the British war effort, stating that they did not want to build a free India from the ashes of Britain. However, opinions were divided. Due to the British policy of limiting investment in India and using the country as a market and source of revenue, the Indian army was relatively weak, poorly equipped, and poorly trained, and the British government was forced to contribute to the Indian budget, while taxes were increased dramatically and the cost of living doubled. While some Indian businesses benefited from increased production during the war, businesses generally felt "disrespected" by the government, especially by the British Raj's refusal to give Indians a greater role in organizing and mobilizing the economy for wartime production. Subhas Chandra Bose commented that "the Quit India Movement opened a new chapter in the Indian freedom struggle." After the outbreak of World War II, Bose formed the Indian Legion in Germany, reorganized the Indian National Army with Japanese support, and launched a guerrilla war against the British authorities, seeking assistance from the Axis powers. The Viceroy, Lord Linlithgow, described this movement as "the most serious rebellion since 1857." In a telegram to Winston Churchill on August 31, he wrote:

" Mob violence is common in large areas of the countryside, and I am quite certain that in September we will see a major attempt to disrupt our war effort once again. The lives of Europeans in remote areas are in danger."

                                                                                     

                                                                                        

When the American Republican presidential candidate Wendell Willkie and YMCA official Sherwood Eddy planned to meet Gandhi, Linlithgow considered it American interference in "our affairs" and asked Churchill to stop them. Indian nationalists knew that the United States supported Indian independence in principle and considered itself an ally. But when Churchill threatened to resign if there was too much pressure, the United States quietly supported him and launched a propaganda campaign against the Indians to boost public support for the war effort. This poorly executed American campaign further alienated the Indians.

The Cripps Mission

In March 1942, amidst growing discontent among Indian soldiers and the general public, and with the war effort in Europe faltering, the British government sent a delegation to India led by Stafford Cripps, the leader of the House of Commons. This mission, known as the Cripps Mission, aimed to secure the full cooperation of the Indian National Congress during the war, in return for transferring and distributing power from the Crown and Viceroy to an elected Indian legislature. The negotiations failed because the Congress's key demands—a timeline for self-government and the specific powers to be transferred—were not addressed.

Factors Contributing to the Outbreak of the Movement

In 1939, with the outbreak of war between Germany and Britain, India—which was a part of the British Empire—also became involved in the conflict. Had a sufficient number of Indian princely states agreed to form a federal government under the terms of the 1935 Act, the Viceroy would not have been able to take the unilateral decision to declare war on India's behalf. Following this declaration, the Congress Working Committee passed a resolution during its meeting on October 10, 1939, condemning the aggressive activities of the Germans. Furthermore, the resolution stated that India could not participate in the war unless it was consulted beforehand. In response to this declaration, the Viceroy issued a statement on October 17, in which he emphasized that Britain was fighting this war with the objective of strengthening peace in the world. He also stated that, after the war, the government would amend the 1935 Act in accordance with the wishes of the Indian people.

Gandhi's reaction to this statement was: "The old 'divide and rule' policy will continue. The Congress asked for bread and received a stone." In accordance with the instructions issued by the High Command, Congress ministers were directed to resign immediately. Complying with these directives, Congress ministers in eight provinces tendered their resignations. The resignation of the ministers proved to be an occasion of great joy and celebration for the leader of the Muslim League, Muhammad Ali Jinnah. He declared this date—December 22, 1939—as the 'Day of Deliverance.' Gandhi urged Jinnah not to celebrate this day, but his appeal proved futile. During the Muslim League session held in Lahore in March 1940, Jinnah declared in his presidential address that the Muslims of the country desired a separate electorate—namely, Pakistan.

Meanwhile, significant political developments unfolded in England. Churchill succeeded Chamberlain as Prime Minister. This meant that the Marquis of Zed land—who had played a pivotal role in securing the passage of the 1935 Act (a measure with which Churchill was deeply dissatisfied)—resigned from his post as the Secretary of State for India. Amidst the deteriorating war situation, and with the objective of appeasing the Indian public, the Conservative Party found itself compelled to concede to certain demands put forth by the Indians. On August 8, the Viceroy issued a statement that subsequently came to be known as the "August Offer." However, the Congress rejected this proposal, and subsequently, the Muslim League also turned it down.

Amidst the atmosphere of widespread discontent arising from the rejection of the Congress's demands, Gandhiji presented his plan to launch a 'Individual Civil Disobedience Movement' during a meeting of the Congress Working Committee held in Wardha. Once again, regarding Satyagraha as the most effective weapon for waging a struggle against the British, the people embraced it wholeheartedly. This weapon was employed on a massive scale to protest against the obstinate attitude of the British. Gandhiji's disciple, Vinoba Behave, was chosen to initiate this movement. Anti-war speeches began to reverberate across every corner of the country; Satyagrahis issued fervent appeals to the public not to cooperate with the government in its war-related endeavors. As a result of this Satyagraha campaign, approximately fourteen thousand Satyagrahis were arrested. On December 3, 1941, the Viceroy ordered the release of all Satyagrahis. Following the Japanese attack on Pearl Harbor, the war situation became even more critical, and the Congress felt the need to re-evaluate its agenda. Consequently, the movement was withdrawn.

The arrival of the 'Cripps Mission' in March 1942—and its subsequent failure—also played a pivotal role in Gandhiji's call for the 'Quit India Movement.' With the objective of resolving the political deadlock, the British government dispatched Sir Stafford Cripps to India on March 22, 1942, to engage in negotiations with Indian political parties and secure their support for Britain's war efforts. A draft declaration was presented on behalf of the British government, containing proposals such as the granting of 'Dominion' status, the formation of a 'Constituent Assembly,' and the right for provinces to frame their own separate constitutions. However, these proposals were to be implemented only after the conclusion of the Second World War. According to the Congress, this declaration offered India but a single promise—a promise that was to be fulfilled at some future date. Commenting on this, Gandhiji remarked, "This is a 'post-dated cheque' on a bank that is itself on the verge of bankruptcy." Other factors contributing to this movement included the threat of a Japanese invasion of India, and the realization among national leaders that the British government was completely incapable of defending the country.

Human health: physical health, mental health, social health | Ayurveda and Global Health.

 

What is human health?

A relative state in which an individual is able to function effectively—physically, mentally, socially, and spiritually—thereby enabling them to express the full range of their unique capabilities within the environment in which they live. In the words of René Dubos, "Health is primarily a measure of each individual's capacity to do what he wants to do and to become what he wants to become."

Current perspectives on health and illness view health as something far more comprehensive than merely the absence of disease. It is understood that human beings are dynamic entities whose health status can fluctuate from day to day, or even from hour to hour. It is more appropriate to view each individual as situated along a graduated scale or a continuous spectrum—a scale that ranges from clearly severe illness, passes through a state characterized by the absence of any apparent disease, and ultimately reaches a state of optimal functioning in every aspect of life. High-level wellness is described as a dynamic process in which an individual actively engages in moving toward the realization of their full potential.

The World Health Organization (WHO) defined health in 1948 as follows:

1) Health means being in a state of complete physical, mental, and social well-being (not merely the absence of disease).

Or,

2) Health means an individual's state of complete physical, mental, and social well-being.

Health is not merely the absence of disease. A healthy life is a successful life; it is essential to understand what holistic health means. The meaning of health can vary from person to person. But, generally speaking, being healthy means successfully navigating all the social, physical, and emotional challenges that life presents.

What is Health?

Health is a balance of our physical, mental, and social well-being, which affects the quality of our lives. Health is not just the absence of disease; it encompasses many aspects that contribute to a happy and successful life.

Physical health:

Physical health means that our body organs are functioning properly and that we take regular care of them. This includes a nutritious diet, regular exercise, sufficient sleep, and avoiding tobacco, alcohol, and other harmful substances.

Mental health:

Mental health means having a stable and positive mental state. It involves managing stress, reducing anxiety, maintaining a positive outlook, and fostering healthy social relationships. Mental health is very important in our lives; we must ensure that our thoughts and emotions are directed in a positive and constructive way.

                                                                                 

                                                                                  

Social Health:

Social health means having positive and fulfilling social relationships. This includes nurturing and supportive relationships with family, friends, and the community. Health is not just the absence of disease; it encompasses well-being in all aspects of our lives. Maintaining good health requires regular check-ups, a healthy lifestyle, and a positive mindset.

Therefore, we should view health not merely as the absence of illness, but as a positive and fulfilling state. We should take care of our physical, mental, and social health so that we can live a happy, positive, and fulfilling life.

Ayurveda

Ayurveda is an ancient Indian system of medicine that has been an integral part of Indian culture for thousands of years. The word 'Ayurveda' comes from the Sanskrit words 'Ayur' (life) and 'Veda' (knowledge), meaning 'knowledge of life'. The primary goal of Ayurveda is to achieve and maintain optimal health and well-being. It emphasizes holistic approaches to healthcare, including diet, exercise, and yoga. Ayurveda also believes that a balance of body, mind, and spirit is essential for good health.

This system places great importance on the use of natural remedies, such as herbs, minerals, and plants, and treats illnesses based on their effect on the body. Ayurvedic practitioners identify the root causes of illnesses and recommend appropriate treatments and dietary changes. Ayurveda promotes a healthy lifestyle for maintaining good health and quality of life, emphasizing healthy eating, yoga, meditation, and exercise. Even today, Ayurveda remains an important part of healthcare in India and many other countries, and people continue to use it to improve and maintain their health.

Global Health

Global health is a field of study that examines health issues, processes, and policies from an international perspective. Its main objective is to improve and protect the health of people worldwide.

Some key topics in global health include:

1. Infectious diseases: Research and efforts to prevent and control the spread of infectious diseases globally.

2. Maternal and child health: Studying and researching policies and programs to improve maternal and child health.

3. Food security: Efforts to ensure that people have access to adequate and safe food through food security measures.

4. Vaccination: Efforts to eradicate and prevent dangerous diseases through vaccination programs.

5. Health services: Efforts to ensure access to and availability of appropriate, effective, and affordable health services.

6. Health rights: Development and implementation of health policies that protect individual and social health rights and responsibilities.

7. Epidemic management: Addressing global health challenges such as AIDS, malaria, and tuberculosis, with particular attention to the health of people with low socioeconomic status.

Many international organizations and governments are involved in the field of global health, working to promote and improve health worldwide and ensure equitable health systems. Furthermore, numerous research and study programs in global health are underway, helping to find new and more effective solutions to health problems.

Monsoon - the wind that brings rain | Monsoon systems around the world : Asian Monsoon, The African Monsoon.

                                                                                   

 

The monsoon, or rainy season, refers to the winds that originate over the Indian Ocean and the Arabian Sea and blow towards the southwest coast of India, bringing heavy rainfall to India, Pakistan, Bangladesh, and other regions. These are seasonal winds that are active in the South Asian region for approximately four months, from June to September. The term was first used in the context of British India (present-day India, Pakistan, and Bangladesh) and neighboring countries. It was used to describe the large-scale seasonal winds that blow from the Bay of Bengal and the Arabian Sea, bringing heavy rainfall to the region from the southwest. In hydrology, the term "monsoon" has a broader meaning—it refers to any wind system that brings the majority of rainfall to a region during a particular season. It is important to note that a monsoon does not necessarily mean continuous rainfall. According to this broader definition, other regions of the world, such as North America, South America, sub-Saharan Africa, Australia, and East Asia, can also be considered monsoon regions. The word "monsoon" comes from the Arabic word "mausim," meaning season. The monsoon is entirely dependent on wind patterns. It occurs when the prevailing winds change direction. As these winds move from cooler to warmer regions, they pick up moisture, resulting in rainfall.

Most summer monsoons are characterized by prevailing westerly winds, which bring heavy rainfall. This is because these winds carry a high amount of moisture as they rise. However, the intensity and duration of these monsoons vary from year to year. In contrast, winter monsoons are dominated by easterly winds, which tend to descend and spread out, resulting in generally dry weather.

Monsoon systems around the world

The major monsoon systems in the world include those of West Africa and Asia-Australia. There is still debate about whether the monsoon systems of North America and South America should also be included in this category.

Asian Monsoon

The intensification of the Asian monsoon has been linked to the uplift of the Tibetan Plateau following the collision of the Indian subcontinent with Asia approximately 50 million years ago. Based on records from the Arabian Sea and studies of wind-blown dust deposits on China's Loess Plateau, many geologists believe that the monsoon first intensified around 8 million years ago. More recently, studies of plant fossils in China and long-term sediment records from the South China Sea suggest that the monsoon originated 15–20 million years ago and was associated with the early uplift of Tibet. To test this hypothesis, samples collected from the deep ocean by the 'Integrated Ocean Drilling Program' are currently being awaited. Since that time, the intensity of the monsoon has undergone significant fluctuations, driven primarily by global climate change—specifically, the cycles of the Pleistocene Ice Age. A study of Asian monsoon climate cycles during the Elmien interglacial period—which spanned from 123,200 to 121,210 years BP (Before Present)—reveals that their average duration was approximately 64 years, with a minimum duration of about 50 years and a maximum of around 80 years—a pattern that closely resembles the pattern observed today.

A study of marine plankton revealed that the South Asian Monsoon (SAM) intensified approximately five million years ago. Subsequently, during the Ice Age, sea levels dropped, and the Indonesian Seaway closed. When this occurred, the flow of cold water from the Pacific Ocean into the Indian Ocean ceased. It is believed that the monsoon intensified further due to the resulting rise in sea surface temperatures within the Indian Ocean. In 2018, a study examining the variability of the SAM over the past one million years found that, during the Ice Age, monsoon rainfall was significantly lower compared to non-glacial periods like the present day. During the warming period following the Last Glacial Maximum, the Indian Summer Monsoon (ISM) intensified on several occasions—specifically during the time intervals of 16,100–14,600 BP, 13,600–13,000 BP, and 12,400–10,400 BP. This is corroborated by changes in vegetation on the Tibetan Plateau, which indicate increased humidity resulting from the intensification of the ISM. However, for most of the subsequent Holocene epoch, the ISM remained relatively weak; nevertheless, substantial snow accumulation occurred in the Himalayas due to cold air currents brought by westerly winds from the west.

                                                                                   

    

During the Middle Miocene epoch, the July ITCZ ​​(Intertropical Convergence Zone—the region of maximum rainfall) shifted northward, leading to increased precipitation in southern China during the East Asian Summer Monsoon (EASM), while the Indochina region became drier. During the Late Miocene Global Cooling (LMCG)—which spanned from 7.9 to 5.8 million years ago—the East Asian Winter Monsoon (EAWM) intensified further as the sub-Arctic front shifted southward. Approximately 5.5 million years ago, the EAWM experienced a sudden and rapid intensification. From approximately 4.3 to 3.8 million years ago, the EAWM was considerably weaker than it is today; however, around 3.8 million years ago, it underwent a sudden intensification. This occurred because crustal extension caused the Tsushima Strait to widen, thereby increasing the inflow of the warm Tsushima Current into the Sea of ​​Japan. Around 3.0 million years ago, the EAWM—which had previously been highly variable and irregular—became more stable, and its intensity increased further during periods of global cooling and declining sea levels. During the cold phases of glacial epochs (such as the 'Last Glacial Maximum' or LGM), the EASM remained weak, whereas it became more powerful during the interglacial and warm phases of these epochs. Another episode of EAWM intensification occurred approximately 2.6 million years ago, followed by a similar event around 1.0 million years ago. The intensity of the EASM increased during Dalsgaard–Escher events, while it is believed to have diminished during Heinrich events. Following the LGM, as sea levels rose, the influence of the EASM extended even deeper into the interior regions of Asia; Furthermore, during the mid-Holocene epoch (approximately 6,000 years ago), another phase of intensified monsoon activity occurred. This was driven by the influence of 'orbital forcing,' an effect further amplified by the extensive vegetation cover present in the Sahara region at that time, which consequently led to reduced dust emissions from the area. This mid-Holocene period—characterized by the peak strength of the EASM—was associated with the expansion of 'temperate deciduous forest-steppe' and 'temperate mixed forest-steppe' ecosystems in Northern China. Approximately 5,000 to 4,500 years ago (BP), the strength of the East Asian Monsoon began to wane, and it has been steadily weakening ever since. A particularly notable decline in its intensity was recorded approximately 3,000 years ago (BP). Throughout the Holocene epoch, the spatial extent of the EASM underwent several shifts: initially, between 12,000 and 8,000 BP, it shifted southward; subsequently, between approximately 8,000 and 4,000 BP, it expanded northward; and most recently—between 4,000 and 0 BP—it once again retreated southward.

South Asian Monsoon

Indian Monsoon

The monsoon in India depends on the winds that blow from the Indian Ocean and the Arabian Sea towards the Himalayas. When these winds collide with the Western Ghats along India's southwestern coast, they bring heavy rainfall to India and neighboring countries. These winds are active in South Asia from June to September. Generally, the monsoon of any region depends on its climate. India has a tropical climate and is primarily influenced by two types of winds – the northeast monsoon and the southwest monsoon. The northeast monsoon is often called the winter monsoon. These winds blow from land towards the sea, crossing the Indian Ocean, the Arabian Sea, and the Bay of Bengal. Most of the rainfall in India occurs due to the southwest monsoon. The Tropic of Cancer passes through India from east to west, which directly affects the country's climate. Of the three seasons – summer, winter, and monsoon – the monsoon season is often referred to as the rainy season.

Generally, during the monsoon season, the temperature drops, but the humidity (moisture) increases considerably. Humidity plays an important role in meteorology. It is the amount of water vapor present in the atmosphere, which reaches the atmosphere from the earth through various forms of evaporation.

East Asian Monsoon

The East Asian monsoon affects vast areas of Indochina, the Philippines, China, Korea, and Japan. Its main characteristic is a hot, rainy summer and a cool, dry winter. Most of the rainfall occurs within a specific east-west zone, except in eastern China, where the rain extends northeastward to Korea and Japan. This seasonal rainfall is known as May-yu in China, Changma in Korea, and Bai-u in Japan. In southern China and Taiwan, the summer monsoon rains begin with pre-monsoon downpours in early May. From May to August, the summer monsoon progresses, alternating between dry and wet periods. It begins in May over Indochina and the South China Sea, reaches the Yangtze River and Japan by June, and finally extends to northern China and Korea by July. The monsoon season ends in August, and the rainfall retreats southward.

The African Monsoon

The monsoon in West-Sub-Saharan Africa was previously thought to be caused by the seasonal movement of the Intertropical Convergence Zone (ITCZ) and the temperature and humidity differences between the Sahara Desert and the equatorial Atlantic Ocean. It moves northward from the equatorial Atlantic Ocean in February, reaching West Africa by around June 22, and then retreats southward by October. The dry north-westerly trade winds, and their extreme form, the Harmattan, are influenced by the northward movement of the ITCZ, while the southerly winds generated by this movement bring the summer rains. The semi-arid regions of the Sahel and Sudan depend on this pattern for the majority of their annual rainfall.

North American Monsoon

The North American Monsoon (also called NAM) lasts from late June or early July through September. It originates over Mexico and brings rain to the southwestern United States by mid-July. Its influence increases rainfall and humidity in the Sierra Madre Occidental of Mexico, as well as in Arizona, New Mexico, Nevada, Utah, Colorado, western Texas, and California. It extends westward to the peninsular regions and the Transverse Ranges of southern California, but rarely reaches the Pacific coast. The North American Monsoon is also known as the summer monsoon, the southwestern monsoon, the Mexican monsoon, or the Arizona monsoon. It is sometimes called the desert monsoon, as most of its affected area lies within the Mojave and Sonoran Deserts.