2021 Atami landslide

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2021 Atami landslide
Re Hai Tu Shi Liu Bei Hai Zhuang Kuang Shi Cha .jpg
Prime Minister Yoshihide Suga overlooks the damaged area; staining on the white building near the centre gives an impression of the height of the landslide during the incident.
Date3 July 2021 (2021-07-03)
Time10:30 a.m. (JST)
Location Atami, Shizuoka Prefecture, Japan
CauseHeavy rainfall
Deaths27

The Atami landslide was a natural disaster which hit the city of Atami on the 3rd of July in 2021. It was caused by heavy rainfall which resulted in significant damage to the community of Atami in Japan. The debris flow by the landslide resulted in life lost, infrastructure damage and had various health consequences. It was argued that the landslide could have been prevented or better managed by local authorities. The role of climate change is evident especially in a country like Japan that experience heavy rainfall. Better management of land use as well as disaster preparedness are critical to prevent and better manage future landslides in Japan.

Contents

Atami Landslide video [1]

Background

The Atami landslide took place on 3 July 2021, with devastating repercussions. In 2021, there were an estimated 972 landslide disasters in Japan. [2] Prior to the Atami landslide there had been very heavy rainfall from 30 June 2021 with flash floods. [3] The city received a total of 432.5mm of rainfall over the four days prior to 3 July 2021, exceeding the average monthly rainfall of 243mm. [3]

It has been discovered that there was illegal landfill management within the area of Aizomegawa River. A soil mound of over 50m high, that exceeded the permitted size regulations, triggered the landslide due to the excessive rain. [4] [5] Debris flow destroyed and damaged many houses and buildings. [6] Despite issuing an emergency security order, evacuations were not completed swiftly. [3]

There were indications highlighting the possibility of a landslide occurring in the preceding months due to the rainfall patterns and early warning systems. [3] These signs could have been used to evacuate citizens early, specifically the elderly and vulnerable. [3] An additional learning outcome from this event is that landfill sites need to be monitored and investigated to ensure compliance with local guidelines, and prompt action is required from the community and local authorities if non-compliant. [3]

Location

Atami is a pacific coastal city, located 68 miles south east of Tokyo, Japan, in the eastern most tip of the Shizuoka Prefecture and northeast of the Izu Peninsula. It has a total population of 34,280 people and more than 50% of Atami's population is over 60 years old within the area of 61.78km², according to the 2020 census. [7]

2021 Atami landslide
Atami, Japan

Atami is originally known for its hot springs and now attracts tourists with the addition of museums exhibiting Japanese culture and vast variety of ocean water sports. [8] Atami also boasts the Atami Castle, which is one of Japan's newest castles built in 1959. It is based on, and has features of, historic castles but was actually built for its panoramic views and used as a tourist facility. [9]

Japan has extreme wet seasons which last approximately 7.2 months from March to October. [10] The typhoon season is usually between July and October. [2] In Atami, within this period, there is a 32% chance of precipitation, each day. [10] June has been highlighted as the most wet month with an average of 13.3 days having rainfall. However, September has the most rain on average at 260.6mm. [10]

Precipitating factors

Landslides generally result from a combination of decrease in the shear strength and increase in shear stress of slope materials. In the case of the Atami landslide, three factors predominantly contributed to these phenomena- natural factors, human and administrative factors. [3]

Natural factors

Atami City is formed mainly by hills, and most of the houses and the cottages rest on steep slopes. Three days leading up to the landslide, the region experienced a maximum periodic rainfall of 449 mm with a maximum 24-hour rainfall of 260 mm. [3] This prolonged and intense level of rainfall was unseen in previous years. [3] Heavy rainfall combined with the geographic characteristics may have affected slope stability and played an important role in triggering the landslide. [3]

Human factors

The soil along the Atami debris flow path is composed predominantly of lava and pyroclastic fall deposits from the Hakone Volcano, which may have theoretically made this region susceptible to landslides. [11] However, there was also a landfill formed at the head of the Aizomegawa River using illegal and inappropriate construction methods, resulting in inadequate drainage and large amount of sediments, decreasing slope stability. [3]

The Geospatial Information Authority of Japan reported that in the 10 years leading up to the Atami landslide, the area underwent a backfill process with a volume of 56,000 m3, which is equal to the volume of the Atami landslide. [3] In addition, the Atami landslide debris was not composed predominantly of pyroclastic materials, but rather of refilled waste, implying that the Atami landslide was not caused by the inherent soil property of the region, but by the backfill of landfill waste products. [3] [11]

These facts suggest that human factors (construction of a landfill) are also responsible for the Atami landslide. [3] [11]

Administrative factors

In addition to natural factors and human factors, there is evidence that inadequate administrative oversight is also partly responsible for the Atami landslide. [3] [12]

The total volume of the landfill at the head of the Aizomegawa River reached twice the volume than that initially authorized well before the Atami landslide. [12] Also, local regulations require that special measures be taken when the height of the landfill exceeds 15 meters, but no special measures have been taken even when the height exceeded 50 meters. [3]

There are internal administrative documents suggesting that prefectural and city officials were aware these dangers as early as 2008, but were slow and ineffective in taking necessary steps to remove the potentially dangerous factors. [12]

Prefectural and city officials have concluded on multiple occasions in the decade leading up to the landslide that the mound and landfill “will likely pose a risk to the lives and fortunes of residents if it collapses.” and was “at risk of washout and collapse” and that the operator “needs to correct the (situation) immediately”. [12] Local officials have ordered business operators and landowners to rectify these conditions. However, they were not able to reinforce these orders, in part due to lack of cooperation by business operators and land owners, changes in land ownership, and difficulty contacting the responsible personnel's. [12]

Although the local government knew of the conditions of the landfill years before the landslide, it was unable to effectively carry out the measures needed to rectify these conditions. [12] This suggest that weak administrative oversight is also partially responsible for the Atami landslide. [3]

Impact of Atami landslide

Landslides cause significant damage to infrastructure along with many other complications. [3] The Atami landslide had considerable impact on the community of Atami, Japan. [3] As a result, the 2021 Atami landslide left 27 people dead and one person was reported missing. [3] [13] The landslide also accounted for multiple injuries. [3] [11] As a result of the landslide up to 274 disaster cases were reported. [3] Unfortunately the most vulnerable seemed to be the most affected with 60% of the affected population being elderly. [3] Local authorities issued warnings for "life threatening conditions" and unfortunately many people were trapped in their houses. [3]

Impact on infrastructure and the community of Atami

The extent of the damage was contributed to the length of the landslide. The debris flow continued for roughly 2km and the total area affected measured up to 73 400m². [11] The effect on the economy and infrastructure were significant with 128 houses in poor condition. [3] [11] Most houses are aged and in poor condition to start with which meant 50% of fatalities occurred inside buildings or houses. [3] Up to 131 houses were completely demolished by the landslide which continued for almost 2km to the sea. [6] [14]

The extent of damage caused by the Atami landslide was also contributed due to the high slope of almost 400m from starting point to the sea. [11] [15] This meant that many houses were severely damaged as the height of the debris flow surpassed double story houses. [15] The power and velocity created by the slope as well as the long travel distance had significant destructive power. [11]

Damaged houses and infrastructure caused by Atami landslide Abandoned in after Atami landslide 04.jpg
Damaged houses and infrastructure caused by Atami landslide

Due to the landslide the power supply was interrupted and left most people without access to water. [3] As a result of the floods and landslide almost 600 people were displaced and had to sought after alternative housing options. [3] Most people had to resort to temporary housing or staying with familiar people like family and friends. [3] Almost a year later up to 144 people still had to take up interim housing. [3]

Preparations and local regulations were not optimal which contributed to the increased effect and impact of the landslide on Atami. [3]

Impact and consequences on health

Short-term consequences

- Crush injuries is a common complication after landslides due to the significant load of the debris. [17] The landslide resulted in multiple injuries and 27 deaths. [3] [11]

- Infectious diseases is a common phenomena after landslides due to contamination of water supplies by the debris flow. [17] Water supply was interrupted by the Atami landslide, yet no reports were released on the increase of infectious diseases.

- Water and sanitation were interrupted by the Atami landslide which increase the risk of infectious diseases. [3] [17] Many people of the community did not have access to clean water to drink for several days after the landslide. [3]

Long-term consequences

- Mental health: Post-traumatic stress disorder is common after landslides. [17] A lack of family support were prevalent due to hundreds of people displaced after the landslide, which also has an effect on mental health. [3] [17] Minimal reports and follow-up were done to screen the mental state of survivors of the Atami landslide.

- Healthcare system: Damage to hospitals and clinics lead to a loss of resources and health care workers. [17] Luckily, disaster management assistant teams (DMAT) were able to access victims and transport them to hospitals. [18]

- The risk for vector borne diseases are increased due to long term environmental changes caused primarily by the alterations in river flow and deforestation. [17] Long term effects on vector borne diseases are yet to be determined after the Atami landslide.

Ecological effects of landslide

The landslide resulted in significant damage of local plant life/ flora which ultimately formed part of the debris flow. [11]

Roads blocked after Atami landslide Road blocked by Atami landslide.jpg
Roads blocked after Atami landslide

Transportation and accessibility

Roads and railway tracks were affected by the debris flow which ultimately effected public transportation. [15] The damage to transportation and public roads effected accessibility to multiple essential services such as hospitals for the community of Atami. [15] Although the DMAT's were able to access the community to provide assistance during the disaster and they continued to provide assistance for almost 14 days after. [18]

Local and international responses

Local responses

Emergency relief operations

In the immediate aftermath of the disaster, Japan's emergency services went into action, with firefighters, police, and the Self-Defense Forces conducting search and rescue operations. Approximately 1,300 search and rescue personnel were involved in rescue and recovery efforts. [20] During the search and rescue period, after heavy rainfall, despite the difficult search and rescue conditions, searchers used drones and heavy machinery to clear debris and search for survivors.

Evacuation and shelter support

Local authorities established emergency shelters as a means of accommodating displaced families. However, due to the large number of evacuees, it was a challenge to control overcrowding and ensure that the shelters had enough space for the residents. In the end, approximately 570 residents took refuge in nearby public facilities. Meanwhile Japan's emergency services provided these residents with basic needs such as food, medical care and security. [21]

Post-disaster investigations and legal actions

After the 2021 Atami landslide, investigations revealed that illegal dumping of dirt and poor construction methods were responsible for the disaster. [22] Mounds of earth were improperly constructed and did not have adequate drainage systems, thus making them more prone to collapse during heavy rains. In addition, the Government took legal action against those responsible, emphasizing the policy implications and committing itself to stricter enforcement of construction and land-use regulations.

Recovery and reconstruction efforts

After the Atami landslide in 2021, the Japanese government invested significant resources in reconstruction. Reconstruction efforts have focused on restoring basic infrastructure, such as roads and utilities, and providing financial support to affected residents. [22] At the same time, authorities have implemented stricter land-use regulations and conducted extensive reviews of similar development projects across the country to prevent future disasters. Monitoring systems and early warning technologies are being improved, and the Government has prioritised sustainable development to reduce the vulnerability of high-risk areas to landslides. In addition, the Government of Japan had begun research and development of emerging technologies to open up geospatial information data, which provided richer information experience and better post-disaster protection measures. This technology provides better information and experience, as well as better post-disaster protection measures, and better assistance for post-disaster health care and people's well-being. [23]

International responses

Condolences and support

In the wake of the Atami 2021 landslide in Japan, there have been expressions of condolence and support from around the globe. United Nations Secretary-General António Guterres also picked up on the incident and offered his condolences. [24]

Media coverage and appeals

In terms of media coverage, in addition to the detailed news of the landslides on the island of Atami, the international media highlighted the wider impacts of climate change, a disaster that has prompted the media to focus on the growing challenges posed by climate change and extreme weather events.

Lessons emerged from disaster

The Atami landslide, caused by heavy rainfall and compounded by human activity, provides several critical lessons for disaster risk reduction, urban planning, and climate adaptation. The key insights are as follows:

Improper land use and its consequences

The disaster investigation revealed that excessive and unregulated accumulation of soil and debris in a designated residential development area significantly exacerbated the landslide. [11] These actions increased slope instability and amplified the debris flow's destructive impact. This underscores the necessity of stricter enforcement of land-use regulations and regular inspections, especially in areas with steep terrain and high rainfall. [15]

Role of climate change in increasing risk

The intensity and frequency of torrential rains in Japan have been rising, consistent with global climate change patterns. Atami experienced 310 millimeters of rainfall in 48 hours, far exceeding safe thresholds. This emphasizes the need to incorporate climate resilience into urban planning and infrastructure design, especially in regions prone to hydrological and geological hazards. [15]

Importance of disaster prepardness

The event highlighted gaps in local preparedness, particularly in early evacuation and communication systems. Despite the warnings of "life-threatening conditions," many residents were caught unaware. Enhanced community-based disaster preparedness programs, clear evacuation protocols, and robust early warning systems are crucial to reducing casualties in similar future events. [23]

Technological integration for risk assesment

Advanced technologies played a pivotal role in post-disaster investigations. Ring shear tests and computer simulations were conducted to analyze soil behavior and flow dynamics. [23] These tools provided a clearer understanding of the causes and effects of the landslide, showing the value of integrating cutting-edge science into disaster risk management. [23]

Advancing open data and collaborative governance

The disaster emphasized the importance of open data initiatives and collaborative governance to improve disaster resilience. Making geo-spatial, hydrological, and urban planning data accessible can help communities and governments co-develop risk reduction strategies. Effective use of open governance frameworks ensures transparency and enhances trust between stakeholders. [23]

Related Research Articles

<span class="mw-page-title-main">Landslide</span> Natural hazard involving ground movement

Landslides, also known as landslips, or rockslides, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, mudflows, shallow or deep-seated slope failures and debris flows. Landslides occur in a variety of environments, characterized by either steep or gentle slope gradients, from mountain ranges to coastal cliffs or even underwater, in which case they are called submarine landslides.

<span class="mw-page-title-main">Flood</span> Water overflow submerging usually-dry land

A flood is an overflow of water that submerges land that is usually dry. In the sense of "flowing water", the word may also be applied to the inflow of the tide. Floods are of significant concern in agriculture, civil engineering and public health. Human changes to the environment often increase the intensity and frequency of flooding. Examples for human changes are land use changes such as deforestation and removal of wetlands, changes in waterway course or flood controls such as with levees. Global environmental issues also influence causes of floods, namely climate change which causes an intensification of the water cycle and sea level rise. For example, climate change makes extreme weather events more frequent and stronger. This leads to more intense floods and increased flood risk.

<span class="mw-page-title-main">Natural disaster</span> Type of adverse event

A natural disaster is the very harmful impact on a society or community after a natural hazard event. Some examples of natural hazard events include avalanches, droughts, earthquakes, floods, heat waves, landslides, tropical cyclones, volcanic activity and wildfires. Additional natural hazards include blizzards, dust storms, firestorms, hails, ice storms, sinkholes, thunderstorms, tornadoes and tsunamis. A natural disaster can cause loss of life or damage property. It typically causes economic damage. How bad the damage is depends on how well people are prepared for disasters and how strong the buildings, roads, and other structures are. Scholars have been saying that the term natural disaster is unsuitable and should be abandoned. Instead, the simpler term disaster could be used. At the same time the type of hazard would be specified. A disaster happens when a natural or human-made hazard impacts a vulnerable community. It results from the combination of the hazard and the exposure of a vulnerable society.

<span class="mw-page-title-main">Lahar</span> Volcanic mudslide

A lahar is a violent type of mudflow or debris flow composed of a slurry of pyroclastic material, rocky debris and water. The material flows down from a volcano, typically along a river valley.

<span class="mw-page-title-main">Atami</span> City in Chūbu, Japan

Atami is a city located in Shizuoka Prefecture, Japan. As of 1 May 2019, the city had an estimated population of 36,865 in 21,593 households and a population density of 600 persons per km2. The total area of the city is 61.78 square kilometres (23.85 sq mi).

<span class="mw-page-title-main">Geological hazard</span> Geological state that may lead to widespread damage or risk

A geologic hazard or geohazard is an adverse geologic condition capable of causing widespread damage or loss of property and life. These hazards are geological and environmental conditions and involve long-term or short-term geological processes. Geohazards can be relatively small features, but they can also attain huge dimensions and affect local and regional socio-economics to a large extent.

<span class="mw-page-title-main">Mass wasting</span> Movement of rock or soil down slopes

Mass wasting, also known as mass movement, is a general term for the movement of rock or soil down slopes under the force of gravity. It differs from other processes of erosion in that the debris transported by mass wasting is not entrained in a moving medium, such as water, wind, or ice. Types of mass wasting include creep, solifluction, rockfalls, debris flows, and landslides, each with its own characteristic features, and taking place over timescales from seconds to hundreds of years. Mass wasting occurs on both terrestrial and submarine slopes, and has been observed on Earth, Mars, Venus, Jupiter's moon Io, and on many other bodies in the Solar System.

<span class="mw-page-title-main">Mudflow</span> Form of mass wasting

A mudflow, also known as mudslide or mud flow, is a form of mass wasting involving fast-moving flow of debris and dirt that has become liquified by the addition of water. Such flows can move at speeds ranging from 3 meters/minute to 5 meters/second. Mudflows contain a significant proportion of clay, which makes them more fluid than debris flows, allowing them to travel farther and across lower slope angles. Both types of flow are generally mixtures of particles with a wide range of sizes, which typically become sorted by size upon deposition.

<span class="mw-page-title-main">Vargas tragedy</span> 1999 natural disaster in Venezuela

The Vargas tragedy was a natural disaster that occurred in Vargas State, Venezuela on 15 December 1999, when torrential rains caused flash floods and debris flows that killed tens of thousands of people, destroyed thousands of homes, and led to the complete collapse of the state's infrastructure. According to relief workers, the neighborhood of Los Corales was buried under 3 metres (9.8 ft) of mud and a high percentage of homes were simply swept into the ocean. Entire towns including Cerro Grande and Carmen de Uria completely disappeared. As much as 10% of the population of Vargas died during the event.

<span class="mw-page-title-main">Mandakini River</span> River in India

The Mandakini River is a tributary of the Alaknanda River in the Indian state of Uttarakhand. The river runs for approximately 81 kilometres (50 mi) between the Rudraprayag and Sonprayag areas and emerges from the Chorabari Glacier. The Mandakini merges with river Songanga at Sonprayag and flows past the Hindu temple Madhyamaheshwar at Ukhimath. At the end of its course it drains into the Alaknanda, which flows into the Ganges.

There have been known various classifications of landslides. Broad definitions include forms of mass movement that narrower definitions exclude. For example, the McGraw-Hill Encyclopedia of Science and Technology distinguishes the following types of landslides:

<span class="mw-page-title-main">Earthflow</span>

An earthflow is a downslope viscous flow of fine-grained materials that have been saturated with water and moves under the pull of gravity. It is an intermediate type of mass wasting that is between downhill creep and mudflow. The types of materials that are susceptible to earthflows are clay, fine sand and silt, and fine-grained pyroclastic material.

<span class="mw-page-title-main">Wildfire emergency management</span>

Wildfires are outdoor fires that occur in the wilderness or other vast spaces. Other common names associated with wildfires are brushfire and forest fire. Since wildfires can occur anywhere on the planet, except for Antarctica, they pose a threat to civilizations and wildlife alike. In terms of emergency management, wildfires can be particularly devastating. Given their ability to destroy large areas of entire ecosystems, there must be a contingency plan in effect to be as prepared as possible in case of a wildfire and to be adequately prepared to handle the aftermath of one as well.

<span class="mw-page-title-main">2014 Hiroshima landslides</span> Natural disaster in Japan

On 20 August 2014, Hiroshima Prefecture in Japan was struck by a series of landslides following heavy rain. The rain triggered 166 slope failures which included 107 debris flows and 59 shallow slides. The landslides hit residential areas including Kabe, Asakita Ward, Yagi, Yamamoto, Midorii, and Asaminami Ward. Of these areas, the Asakita and Asaminami Wards in Northern Hiroshima were hit the hardest.

<span class="mw-page-title-main">2016–2017 Zimbabwe floods</span>

Zimbabwe experienced severe floods from December 2016 through March 2017 due to heavy rains that followed a two-year drought.

<span class="mw-page-title-main">Climate change in the Philippines</span> Impact of climate change on the Philippines

Climate change is having serious impacts in the Philippines such as increased frequency and severity of natural disasters, sea level rise, extreme rainfall, resource shortages, and environmental degradation. All of these impacts together have greatly affected the Philippines' agriculture, water, infrastructure, human health, and coastal ecosystems and they are projected to continue having devastating damages to the economy and society of the Philippines.

<span class="mw-page-title-main">2020 Kerala floods</span> Indian flood

During the heavy rainfall over the monsoon period from 1 June to 18 August 2020, all 14 districts in Kerala were affected with 104 dead and 40 injured. Four districts in Kerala were flooded on 7 August 2020. Major reported incidents in relation to flooding include a landslide in Idukki district on 6 August, claiming 66 lives and an Air India plane crash that caused the death of 21 people. The 2020 flood in Kerala marked the third year in a row of severe monsoon flooding.

<span class="mw-page-title-main">Urban flooding</span> Type of flood event in cities

Urban flooding is the inundation of land or property in cities or other built environment, caused by rainfall or coastal storm surges overwhelming the capacity of drainage systems, such as storm sewers. Urban flooding can occur regardless of whether or not affected communities are located within designated floodplains or near any body of water. It is triggered for example by an overflow of rivers and lakes, flash flooding or snowmelt. During the flood, stormwater or water released from damaged water mains may accumulate on property and in public rights-of-way. It can seep through building walls and floors, or backup into buildings through sewer pipes, cellars, toilets and sinks.

<span class="mw-page-title-main">2016 Pakistan Floods</span> Natural disaster in Pakistan

In 2016 Pakistan experienced higher rainfall than normal (10-20%), especially in the pre-monsoon season. Heavy monsoon rains are common in the region. This led to multiple periods of flooding, landslides, and damage particularly in Northern Pakistan. The Swat River overflowed and multiple landslides occurred around Pakistan including in Khyber Pakhtunkhwa, Gilgit-Baltistan, Azad Jammu, and Kashmir.

From January 31 to February 1, 2022, heavy rainfall impacted Ecuador, which caused multiple landslides, floods, and mudflows. It was caused by the country's biggest rainfall in nearly 20 years, which fell on the capital.

References

  1. Deng, Francis; Cheng, Jeffrey (20 June 2017), "Operculum diagram (wikimedia commons)", Radiopaedia.org, doi: 10.53347/rid-54033 , retrieved 28 November 2024
  2. 1 2 "Japan: number of landslide disasters 2021". Statista. Retrieved 22 November 2024.
  3. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 Poudel, Namita; Chi, Guo; Yuqiu, Cao; Shaw, Rajib (27 June 2024). "Atami landslides 2021 Japan: Landfill issues, elderly casualties, key lessons and challenges". Natural Hazards Research. doi: 10.1016/j.nhres.2024.06.006 . ISSN   2666-5921.
  4. "Two years after Atami landslide, dangerous soil mounds exist". The Asahi Shimbun. Retrieved 21 November 2024.
  5. "Atami mudslides: landfill soil may have triggered the disaster | NHK WORLD-JAPAN News". NHK WORLD. Retrieved 16 November 2024.
  6. 1 2 "Asian Disaster Reduction Center(ADRC)". www.adrc.asia. Retrieved 16 November 2024.
  7. "Atami (Shizuoka , Japan) - Population Statistics, Charts, Map, Location, Weather and Web Information". www.citypopulation.de. Retrieved 19 November 2024.
  8. Organization, Japan National Tourism. "Atami & Ito | Shizuoka | Tokai | Destinations | Travel Japan - Japan National Tourism Organization (Official Site)". Travel Japan. Retrieved 19 November 2024.
  9. Organization, Japan National Tourism. "Atami Castle | Travel Japan - Japan National Tourism Organization (Official Site)". Travel Japan. Retrieved 19 November 2024.
  10. 1 2 3 "Check Average Rainfall by Month for Atami". World Weather & Climate Information. Retrieved 19 November 2024.
  11. 1 2 3 4 5 6 7 8 9 10 11 Zhang, Shuai; Wang, Fawu; Li, Ran (9 January 2022). "First insight into the catastrophic Atami debris flow induced by a rain gush on 3 July 2021 in Shizuoka, Japan". Springer Nature 2021. 19 (2): 527–532. Bibcode:2022Lands..19..527Z. doi:10.1007/s10346-021-01788-1. ISSN   1612-510X.
  12. 1 2 3 4 5 6 Itabashi, Hiroyoshi; Kawashima, Kae (18 October 2021). "Atami knew of landslide risk but slow to move on problem". The Asahi Shimbun.
  13. Yamazaki, Fumio; Liu, Wen (16 July 2023). "Damage Assessment of Debris Flow in Atami City, Japan, Based on Field Survey and High-Resolution SAR Data". IGARSS 2023 - 2023 IEEE International Geoscience and Remote Sensing Symposium. IEEE. pp. 2354–2357. doi:10.1109/IGARSS52108.2023.10282449. ISBN   979-8-3503-2010-7.
  14. Yanagawa, Youichi; Jitsuiki, Kei; Nagasawa, Hiroki; Ohsaka, Hiromichi; Ishikawa, Kouhei (1 January 2022). "Questions Regarding the Initial Request for the Dispatch of Disaster Medical Assistance Teams for a Landslide after Torrential Rain at Izuyama in Atami, Japan". Journal of Emergencies, Trauma, and Shock. 15 (1): 71–72. doi: 10.4103/jets.jets_123_21 . ISSN   0974-2700. PMC   9006723 . PMID   35431485.
  15. 1 2 3 4 5 6 IMAIZUMI, Fumitoshi; OSANAI, Nobutomo; KATO, Shinyu; KOIKE, Masaru; KOSUGI, Ken'ichirou; SAKAI, Yusuke; SAKAGUCHI, Hiroshi; SATOFUKA, Yoshifumi; TAKAYAMA, Shoki; TANAKA, Takafumi; NISHI, Yotaro (6 June 2022). "Debris flow disaster in Atami, Japan, in July 2021". International Journal of Erosion Control Engineering. 15 (1): 1–6. doi: 10.13101/ijece.15.1 . ISSN   1882-6547.
  16. 番記者 (10 December 2021), 日本語: 2021 Damage to infrastructure and buildings after Atami Landslide , retrieved 26 November 2024
  17. 1 2 3 4 5 6 7 Kennedy, Iain T R; Petley, Dave N.; Williams, Richard; Murray, Virginia (2015). "A Systematic Review of the Health Impacts of Mass Earth Movements (Landslides)". PLOS Currents. 7. doi: 10.1371/10.1371/currents.dis.1d49e84c8bbe678b0e70cf7fc35d0b77 . ISSN   2157-3999.
  18. 1 2 Yanagawa, Youichi; Kanda, Akio; Taniguchi, Hiroaki; Muramatsu, Ken-ichi; Sakai, Tatsuro; Nagasawa, Hiroki; Takeuchi, Ikuto; Ohsaka, Hiromichi; Omori, Kazuhiko (2024). "Comparison of the Utilization of Disaster Medical Assistance Teams (DMATs) and Multiple Physician-staffed Helicopters in Mass Casualty Responses". Disaster Medicine and Public Health Preparedness. 18. doi:10.1017/dmp.2024.188. ISSN   1935-7893.
  19. 番記者 (10 December 2021), 日本語: 2021 Roads blocked after Atami landslide , retrieved 26 November 2024
  20. "Japan Landslide Death Toll Rises to 15". Voice of America. 18 July 2021. Retrieved 15 November 2024.
  21. Tada, Shinya; Jitsuiki, Kei; Ohsaka, Hiromichi; Yanagawa, Youichi (10 December 2021). "Benefits and Drawbacks of Using Hotels as Shelters After a Landslide". Disaster Medicine and Public Health Preparedness. 16 (5): 1851–1854. doi:10.1017/dmp.2021.335. ISSN   1935-7893. PMID   34889180.
  22. 1 2 "Massive Soil Mound on Slope Seen as Worsening Japan Mudslide". Voice of America. 7 July 2021. Retrieved 15 November 2024.
  23. 1 2 3 4 5 Kanbara, Sakiko; Shaw, Rajib (21 December 2021). "Disaster Risk Reduction Regime in Japan: An Analysis in the Perspective of Open Data, Open Governance". Sustainability. 14 (1): 19. doi: 10.3390/su14010019 . ISSN   2071-1050.
  24. Dujarric, Stéphane. "Statement attributable to the Spokesperson for the Secretary-General - on Japan". www.un.org. Retrieved 15 November 2024.