On May 10, an area of low pressure was identified over the Arabian Sea roughly 400 km (250 mi) to the northwest of the Maldives. Moving northwestward, it gradually organized, becoming a depression during by the evening of May 12. After turning more toward the west, the system continued to slowly deepen. On May 14, the S.S. Kampala sailed into the system, encountering 55 km/h (35 mph) winds and rough seas. Over the following two days, the depression intensified into a cyclonic storm, with gale-force winds extending 150 km (90 mi) from the center. During the overnight hours of May 16 through 17, the S.S. Mohammedi sailed almost directly into the center of the cyclone, reporting a barometric pressure of 974 mbar (hPa; 28.77 inHg) and 9.1 m (30 ft) waves. Several other vessels, such as the S.S. Saudi and S.S. Exchequer, encountered the storm. Both ships reported hurricane-force winds, and the latter endured seas as high as 15.2 m (50 ft) early on May 18. Later that day, the storm weakened so rapidly the crew of the S.S. Exchequer were able to watch the pressure on their barometer actively rise. Continuing westward, the system degraded to a remnant low before dissipating on May 19 off the coast of Hadhramaut, Yemen.
As a developing cyclone, the system brought monsoon-like moisture to much of the Maldives, Ceylon (present-day Sri Lanka), and southern India between May 14 and 17. The heaviest rains fell on May 17, with 190 mm (7.5 in) recorded at Kochi, India, that day.
On May 25, an upper-level low pressure system developed over the northern Bay of Bengal. The following day, a surface low formed in association with this feature. By May 27, the low further consolidated into a depression while situated 285 km (175 mi) south of Kolkata, India. Tracking northward, it intensified into a deep depression before making landfall on the Sundarbans region of West Bengal—near the border of East Pakistan—early on May 28. Though it was classified a deep depression, stronger winds of up to 75 km/h (45 mph) were reported from Sagar Island. Based on measurements from nearby stations, it is estimated that the system attained a minimum pressure of 988 mb (hPa; 29.18 inHg) just as it moved ashore. Once inland, the system quickly weakened and accelerated northeastward. It later dissipated over Assam on May 30.
The system produced torrential rains across eastern India and East Pakistan. In Cherrapunji, 540 mm (21 in) of rain fell during a two-day span, while many other areas recorded over 100 mm (3.9 in). No rainfall data were available from West Bengal and Assam. Strong winds from the storm destroyed numerous homes in West Bengal, and at least seven people were killed.
On June 29, a trough, associated with an upper-level low, extended over the northwestern Bay of Bengal. Following a drop in sea-level pressure over the next day, a depression formed in this area. Moving slowly westward, the storm intensified into a deep depression early on July 2. Shortly thereafter, the system made landfall near Angul, India, and accelerated toward the northwest. The system later dissipated on July 4 over Madhya Pradesh after being absorbed back into the trough that it developed from.
Widespread heavy rains accompanied the depression along portions of the coast from Orissa to West Bengal and as far inland as Madhya. Sagar Island recorded at least 360 mm (14 in) of rain over the span of two days, while Vishakhapatnam received 300 mm (12 in) in just one. As much as 100 mm (3.9 in) of precipitation fell across Madhya Pradesh.
On June 26, a slow-moving trough developed over Gujarat. By July 2, the system developed into a shallow land depression while situated 80 km (50 mi) north of Veraval. Winds in the area were measured up to 45 km/h (30 mph); however, as the system moved offshore, winds quickly increased to 65 km/h (40 mph). Low pressures were recorded across the area, with a minimum of 990.8 mbar (hPa; 29.26 inHg) measured in Dwarka. Becoming nearly stationary off the coast of Gujarat, the depression began to interact with an approaching monsoon. This interaction caused winds to increase, with two vessels reporting 75 km/h (45 mph) winds during the late morning hours of July 4. Later that day, the system began moving to the northwest and quickly weakened. It was last noted the following day as a dissipating low over the northeastern Arabian Sea.
Between July 2 and 4, heavy rains amounting to more than 300 mm (12 in) fell across much of the Saurashtra region of Gujarat. These rains triggered severe flooding that killed at least 35 people and left 6,000 others homeless. At least 500 homes were destroyed in the region.
On August 6, a westward moving area of low pressure was identified over Burma. Initially an upper-level system, it gradually propagated to the surface, becoming a depression on August 9. Tracking west-northwestward, the system crossed the Indian coastline later that day near Balasore, where a pressure of 996.1 mbar (hPa; 29.42 inHg) was measured. Sustained winds reached just 30 km/h (15 mph). Once onshore, the depression degenerated into a remnant low on August 10. The remnants continued northwestward, ultimately merging with a trough over Uttar Pradesh on August 12.
The depression dropped heavy rains over parts of India between August 8 and August 14. The highest totals were recorded on August 14 when 240 mm (9.4 in) of rain fell in Jhansi. Significant flooding took place along the Ganges River as a result of the rains. Forty villages along the river near Fatehgarh were inundated.
As the previous depression dissipated over India, a new circulation developed over the Bay of Bengal on August 12. This system quickly became a depression. Moving slowly northwestward, it became a deep depression on August 14 before making landfall in the Sundarbans region. Winds up to 45 km/h (30 mph) were reported in Sandheads. Once onshore, it turned westward and slowed while maintaining its intensity. The system finally weakened on August 18 as it resumed moving northwestward again, and two days later it dissipated over southeastern Rajasthan.
Large portions of India were affected by rains from the depression, with Orissa and Madhya receiving the heaviest rains. According to Prime Minister Jawaharlal Nehru, up to 1,000 mm (40 in) of rain fell across portions of Orissa. The tremendous precipitation triggered disastrous floods that killed at least 65 people. Continued rains over the next two weeks exacerbated the situation and by August 30, an estimated 2.5 million people were homeless. Most affected were areas around the Mahanadi River and its tributaries where flood waters reached 3.7 m (12 ft) in depth. At least 85 villages were reportedly destroyed. Orissa government officials described the disaster as "the worst in living memory." Rail lines and roads were severely damaged across the state, hampering initial relief efforts. A total of 1.87 million acres of crops were flooded and overall damage amounted to 7008111700000000000♠₹112 million.
On August 20, a wave of low pressure formed over Burma. Moving westwards, this upper-level system triggered the development of a surface low two days later over the Bay of Bengal. Turning northwestward, the low consolidated into a depression by August 24 before making landfall in the Sundarbans region later that day. Once onshore, the depression degenerated into a remnant low; the remnants persisted until August 28 when they were absorbed into a trough over Rajasthan Pradesh.
Heavy rains affected much of Bihar, Madhya Pradesh, Punjab, and Uttar Pradesh. The highest daily precipitation total was measured in Ghatsila at 190 mm (7.5 in). These rains triggered severe flooding along the Beas, Ganges, Jamuna, and Sutlej rivers. Large areas of Uttar Pradesh were left submerged, and significant crop and property damage took place in Punjab. At least 55 people were killed in Punjab alone, and losses overall amounted to $9.24 million (1960 USD).
On September 22, an area of low pressure was identified over the Andaman Sea. Tracking northwestward, the system consolidated into a depression two days later over the Bay of Bengal. During the evening of September 24, it further strengthened to a deep depression, with winds of 55 km/h (35 mph). Early the next day it made landfall in Orissa between Balasore and Chandabali. Once onshore, the system slowed and turned northeastward. It later dissipated over Nepal on September 28 as it interacted with the Himalayas.
Heavy rains accompanying the depression affected much of Bihar, Orissa, and West Bengal. Many areas recorded more than 200 mm (7.9 in) during a four-day span; the highest single-day total was 270 mm (11 in) in Bahadurganj.
In late September, a tropical storm developed over the South China Sea. Striking Vietnam, the storm slowly moved over Indochina, ultimately crossing 100°E and entering the basin on October 5 while over Thailand. After crossing southern Burma, the low moved northwestward over the Bay of Bengal and reorganized. Following a report of 45 km/h (30 mph) winds from the S.S. Glenpark on October 8, the system was classified as a depression. Moving slowly northwestwards, the system further deepened into a cyclonic storm on October 9. Several ships in the path of the storm recorded gale-force winds, depicting its strengthening. Early on October 10, it became a severe cyclonic storm and soon reached its peak intensity with winds of 110 km/h (70 mph). Its central pressure at this time was estimated to be 986 mbar (hPa; 29.12 inHg). The National Oceanic and Atmospheric Administration (NOAA) estimated that the storm attained one-minute sustained winds of 155 km/h (100 mph). Turning northeastward, the system made landfall between Barisal and Noakhali in East Pakistan, with the eye passing directly over the islands of Bhola, Hatia, and Ramgati. Once onshore, the system quickly weakened and ultimately dissipated over Assam early on October 12.
Across coastal areas of East Pakistan, the storm wrought catastrophic damage. A 5.8 m (19 ft) tidal surge washed over the islands of Hatia, Sandwip, Kutubdia. Communications across the region were crippled, and it took six days for word of the scale of damage to reach officials. Entire villages were reportedly wiped out by the storm. Approximately 35,000 homes were destroyed, most of which were thatched huts made of bamboo and mud. About 300 schools were also damaged. The worst damage took place on Ramgati Island where 3,500 people were killed. Roughly 95 percent of the island's structure were destroyed, forcing residents to cling to trees for survival. Only two police officers survived and were able to inform government officials of the disaster. An estimated 6,000 people perished while another 100,000 were left homeless. Heavy rain accompanied the storm, with Cox's Bazar reporting 180 mm (7.1 in). Relief efforts in the wake of the storm were hampered by the nation's poor infrastructure and debris left behind. On October 18, members of the East Pakistani military were deployed to the hardest hit areas to provide stable communication and clean drinking water.
On October 26, a trough formed over the south Andaman Sea and extended into the southern Bay of Bengal. By October 28, the system consolidated into a depression as it moved northwestward. Steadily intensifying, several ships encountered the storms increasing winds as it moved northward in the Bay. On October 30, it attained gale-force winds and further became a severe cyclonic storm early the next morning. During the evening of October 31, the IST Barisal recorded winds of 130 km/h (80 mph), indicating that the system had acquired a core of hurricane-force winds. The maximum winds of this system is unknown, though reports indicated that winds peaked between 150 and 215 km/h (90 and 135 mph). NOAA estimated that the storm peaked with one-minute sustained winds of 195 km/h (120 mph) and a pressure of 966.7 mbar (hPa; 28.55 inHg). The storm soon made landfall with great intensity near Noakhali, East Pakistan, just three weeks after the previous storm devastated the country. Once onshore, cold, dry air quickly wrapped around the backside of the cyclone. Within four hours of landfall, little rainfall was reported near the storm's eye. The cyclone rapidly weakened and dissipated the following day over the Lushai Hills.
Striking East Pakistan as a powerful storm, the system produced a storm tide of 6.1 m (20 ft) that moved 16 km (10 mi) inland, devastating many communities. A storm surge of 6.7 m (22 ft) was measured in Halishahar. In addition to the surge, there was a series of tidal waves that followed the storm, causing additional damage. Offshore, these waves were estimated at 12.2 m (40 ft); though they significantly decreased before impacting land. Chittagong and surrounding communities were regarded as the hardest hit, with most being submerged in 3 m (10 ft) of water. The city's port was largely destroyed, with almost every vessel washed ashore. Some were found 16 km (10 mi) away and one even at another port. The storm's intense winds, estimated as high as 240 km/h (150 mph) on Sandwip Island, leveled buildings and scattered debris over large distances. Crops were flattened by the storm and in some instances had been "burnt" by the sheer force of the wind. A total of 14,174 people perished in the storm while another 200,000 were left homeless. Following the mass casualties from the two storms, the Government of Pakistan requested the assistance of former National Hurricane Center director, Gordon E. Dunn, to improve the warning system.
On November 5, an area of low pressure was identified over Lakshadweep. Tracking generally northwestward, it gradually organized into a depression by November 7. No further development took place over the following days and the system eventually degraded into a remnant low on November 10. Though the storm itself did not impact land, associated moisture combined with a low over the Bay of Bengal to produce heavy rains across Madras State and nearby islands from November 5 to 10.
On November 7, an area of low pressure over the Bay of Bengal formed and gradually moved towards India. By November 9, it was located just of the Coromandel Coast. The following day, it deepened into a depression while situated off the northern edge of Ceylon. Becoming nearly stationary, the system failed to develop and soon weakened into a remnant low. The low dissipated early on November 12. Heavy rains fell across much of Madras State in association with the system; a 24‑hour total of 240 mm (9.4 in) was reported in Nagapattinam. These rains triggered significant flooding that disrupted travel and communications. Severe damage took place in Madurai where 10,000 people were left homeless. Overall, five people were killed and 150,000 were left homeless.
On November 14, an area of low pressure formed to the west of Lakshadweep. Tracking generally westward, it eventually developed into a depression three days later. Gradual intensification took place over the following two days, with the system becoming a cyclonic storm on November 19. On November 20, the system attained its peak intensity with winds of 75 km/h (45 mph) and a minimum pressure of 994 mbar (hPa; 29.36 inHg). Continuing westward, the cyclone entered the Gulf of Aden on November 22 before becoming nearly stationary. During this time, it weakened to a depression before dissipating the following day.
A well-defined area of low pressure was identified over the southwestern Bay of Bengal on November 17. The following day, the system developed into a depression as it moved slowly northwestward. On November 20, as it neared the coast of Tamil Nadu, it intensified into a cyclonic storm, with gusts estimated as high as 135 km/h (84 mph). Shortly thereafter, it made landfall near Chennai. In nearby Tambaram, a pressure of 995.7 mbar (hPa; 29.41 inHg) was recorded, the lowest in relation to the cyclone. A small storm, it quickly weakened once onshore and was last noted early on November 21 as a dissipating low.
Heavy rains impacted most of southern Madras State, with a maximum daily total of 110 mm (4.3 in) in Punalur. The most significant damage took place in Madras City where gale-force winds uprooted trees and disrupted transport and communications. Many poorly constructed homes were damaged or destroyed by the storm, leaving numerous low-income families homeless.
On November 24, the S.S. Rajula sailed under a well-defined trough over the southwest Bay of Bengal and reported 55 km/h (35 mph) winds. Two days later, a tropical wave interacted with the system and resulted in the development of a depression. Over the following several days, the system drifted northwestward without change in intensity. By December 3, it degenerated into a remnant low, ultimately tracking over southern India, near Circars, on December 4 before dissipating. The system brought locally heavy rains to parts of the Andaman Islands and Andhra Pradesh.
This is a table of all storms in the 1960 North Indian Ocean cyclone season. It mentions all of the season's storms and their names, durations, peak intensities (according to the IMD storm scale), areas affected, damages, and death totals. Damage and death totals include the damage and deaths caused when that storm was a precursor wave or extratropical low, and all of the damage figures are in 1960 USD.