Exclusive: Unprecedented disasters are here, yet we are still ‘tasting a hundred herbs’

In early October, many parts of Northern China experienced record-breaking rainfall for this period. Amidst the bewilderment of city dwellers asking, “How long will this rain go on?” and “Is the North really becoming the South?”, and as farmers stood heartbroken before crops submerged in mud, we marked the 36th International Day for Disaster Risk Reduction.

Observed on 13 October, the International Day for Disaster Risk Reduction is a UN-established day intended to raise global awareness and prevention of disaster risks. This year’s theme, “Investing in resilience to enhance disaster prevention and reduction capabilities”, emphasises prioritising pre-disaster preparation over post-disaster remedy.

This is common sense—if we know a disaster is coming, everyone prepares. The key is, do we truly understand disasters? Hao Nan, a disaster relief worker, made a comment that seems counter-intuitive: “It is no exaggeration to say that our understanding of disaster impact is still at the ‘Shennong tasting a hundred herbs’ stage.”

His words have a basis. Two months after the catastrophic rains in Xinglong, Hebei, and Miyun, Beijing, and during this National Day holiday, the organisation he belongs to, Zhuoming Xinyuan (hereafter “Zhuoming”), led a team back to the disaster areas. Starting from the heavily damaged Taishitun, they traced the path of the floods to reconstruct the entire disaster process.

How to dissect a disaster the way one would analyse a pathogen’s mechanism of disease—deducing its occurrence through reverse and forward logic and assessing risk—requires not only comprehensive calculations across multiple disciplines but also a social-level analysis of how different stakeholders perceive disasters and their impacts from various perspectives. Hao Nan believes that this work is still far from sufficient. Due to climate change, extreme precipitation andfloods exceeding design standardswill become increasingly common. What happens next? We hope the experiences and dilemmas of the Zhuoming team are seen by more people concerned with meteorological disasters.

◉ During the National Day holiday, the Zhuoming Xinyuan team revisited the disaster-stricken areas of Xinglong County, Hebei. A family home was largely destroyed by a landslide; to this day, the family can only live temporarily in relief tents and shelters made of corrugated iron and wooden boards. They were fortunate: when the flood struck, they managed to take refuge on a stone peak beside the house for several days and survived. Image source: Zhuoming volunteer Xie Yijing

I. The North Becoming the South: Townships Still Forgotten

North China has seen intense rainfall these past few days. As many farmers have lamented, the North is becoming like the South. With extreme rainfall becoming more frequent, what new problems have you encountered in disaster management?
Hao Nan: In recent years, areas naturally prone to flooding have experienced “over-standard” floods—those exceeding design limits—more frequently and intensely. In the future, it won’t just be the rainy South; similar disasters may occur more often in the North. Rather than the North-South divide, when facing floods that exceed design standards, we focus more on the “inter-annual variation rate” and “intra-annual distribution” of river runoff to evaluate the difficulty of prevention. For example, in Taishitun Town, Miyun District, Beijing, the peak flow reached 3,000 cubic metres per second during the extreme rains in late July, yet the usual peak flow during the flood season is only 5–10 cubic metres per second, and the river often dries up outside the flood season.

In the “humid zones” of the South, rivers with high flood risks generally don’t have such extreme variability—flows might be in the thousands or tens of thousands during the flood season and still be around two or three thousand normally, with banks flooding every few years. However, extraordinary floods with return periods of 20–40 years are much harder to prevent—human experience in flood control is difficult to pass down through generations.

The increase in extreme precipitation and over-standard floods is also changing how the government works. “Call-and-response” (alerting lower-level officials) has become a primary task for emergency management departments when dealing with rainstorms and floods. Once a red rainstorm warning is issued and flood response is activated, calls are made down the chain of command to the grassroots level: “(The) heavy rain is coming; get people in high-risk areas to evacuate immediately!” The first time this happens, it is inevitably chaotic.

With climate change, the 400mm isohyet is shifting north. In the future, in mountainous areas with stream and valley terrain between the 400mm and 800mm isohyets, the probability of extreme precipitation leading to severe flash floods and flooding of small-to-medium rivers will increase.

In August 2024, widespread rainstorms and floods in Jianchang County, Huludao City, and other areas led to at least 11 deaths. A team leader who participated in both last year’s Huludao floods in Liaoning and this year’s floods on the Beijing-Chengde border told me that in terms of type, scale, and on-site conditions, the two disasters were remarkably similar.

Can we learn from these disaster areas? Can we realise that it could happen to anyone, and then think about what needs to be done?

◉ Flash floods often surge down gullies and valleys—which are also the same places where terraces and roads are easily constructed. In the typical flash-flood gully terrain shown in the image, if flash floods and debris flows erupt simultaneously in the horizontal river valley in front of a village and the vertical gully behind it, residents in the impacted houses have little chance of escape. Image source: Zhuoming study member Ge Mingning
Following the extreme rainfall in Miyun, we immediately reached out to our food-farming friends in the outskirts of Beijing to understand the impact. However, by 8 October, as North China entered another wave of heavy rain and plummeting temperatures, even a food and agriculture organisation like ours—deeply concerned with the autumn harvest—began to feel a certain “fatigue” regarding the disasters. In your observation, which areas’ disasters deserve more attention in recent years, and are there “blind spots” where devastation goes unnoticed?
Hao Nan: Back in 2013, building on the experience of those before me, I proposed the “Five Imbalances“: imbalance in disaster types, imbalance between major and minor disasters, imbalance between urban and rural areas, imbalance across different post-disaster stages, and imbalance between pre- and post-disaster efforts. These five imbalances in social attention still exist today; nothing has fundamentally changed, except that whereas people once cared more about earthquakes, they are now more concerned with meteorological disasters. The allocation of resources has always been more closely linked to social visibility than to the actual scale of the disaster. Consequently, rural areas consistently receive less attention than cities.

Over the past decade, the trend of climate change leading to more frequent disasters has become obvious. However, the public only truly received a “lesson” during the extreme rainfall and flooding of 23 July 2021 in Henan (often referred to in the media as the “7.20 extreme rainstorms”). On the evening of 20 July, Zhengzhou’s urban area saw 200mm of rain in a single hour. This unprecedented deluge naturally caused severe urban waterlogging, and news of over a dozen citizens drowning in the metro triggered a public outcry. Yet, at the same time—or even slightly earlier—far more severe casualties occurred that few people knew about.

The official death toll for the Zhengzhou floods was 380, 70% of whom were from the hilly towns and counties in Zhengzhou’s suburbs, with deaths concentrated before 1 pm on 20 July. The vast majority perished due to flash floods, geological disasters, and flooding of small-to-medium rivers; only about a tenth died from urban waterlogging. Yet, public discourse focused almost entirely on the cases of urban flooding.

On the other side of the Yellow River in Xinxiang, the extremity of the rainfall around 20 July was no less severe than in Zhengzhou. Although the death toll was lower—as this is primarily a plain where water flows more slowly, allowing more opportunities for escape and rescue—the area was submerged in a vast sea of water. On satellite maps, villages became isolated islands, resembling Lake Poyang during its dry season. According to our preliminary estimates, including Hebi’s Qi and Jun counties where the floodwaters flowed downstream, nearly one million people were trapped by floods, with rescue teams assisting at least 400,000 of them. In the county-level city of Weihui in Xinxiang alone, 200,000 people had to be evacuated.

◉ North of Xinzhuang Village, Jishui Town, Weihui City, Xinxiang: trapped by floods for five days, with torrents rushing through the main village road. The interviewee stated that all single-storey houses were completely submerged. Image source: Zhejiang Economic Television

Hao Nan: After all these years, some critical issues remain undiscussed—the mechanisms and risk types of urban waterlogging are fundamentally different from those of flash floods, geological disasters, and river flooding. The risk of casualties from urban waterlogging is far lower than from flash floods or geological disasters, and the impact of the latter is usually far more profound. Even in Zhengzhou, despite such extreme precipitation, the urban floodwaters were drained in a day, while villages along the downstream rivers remained submerged for over half a month.

Furthermore, urban flooding mainly involves rainwater, which is relatively simple to clear. Urban infrastructure is typically restored within days, and citizens generally do not lose their livelihoods. In contrast, floodwaters rushing down from the mountains carry vast amounts of silt and debris, destroying everything in their path.

During the extreme floods in Qiandongnan Prefecture, Guizhou, this June, the silt mixed with rubbish left behind in Rongjiang city was one to two metres thick. More importantly, mountain floods destroy farmland, roads, and infrastructure. In the heavily hit townships of Xinglong County, Hebei, which we visited, many basic farmlands located in mountain valleys, as well as riverbank fields and terraced fruit trees on the slopes, were washed away. When basic farmland is destroyed by debris flows, it is difficult to reclaim and requires formal de-registration. While farmers receive some subsidies for losing land to disasters, the loss of livelihood is permanent.

In the future, the trend of frequent mountain floods will continue, and may even accelerate.

◉ Gutian Town, Shanghang County, Fujian: heavy rain caused severe landslides. Image source: Zhou Xuan

II. Promoting Disaster Reduction: Who can afford to spend three months drinking with the villagers?

This year’s theme for the International Day for Disaster Risk Reduction focuses on resilience. You have previously emphasised that preventing disasters requires a comprehensive system of early warning, monitoring, and evacuation drills. For example, during the rescue efforts at Dongting Lake in Hunan, local authorities arranged buses in advance for villages where dam breaches were imminent; the villagers were experienced and reacted quickly. In recent years, has there been an increase in funding and awareness for enhancing disaster resilience within China?
Hao Nan: I wonder how OCHA (the UN Office for the Coordination of Humanitarian Affairs, which oversees emergency disaster response) would view this theme. The word “resilience” is frequently used in elite discourse, but ordinary people don’t buy into it. It is discussed across social sciences and engineering, but the concepts and interpretations vary so wildly that it is difficult to establish a unified definition, let alone a method of calculation. Such a broad, vague concept makes it very easy to form a so-called “consensus”. Regarding “disaster resilience”, I believe the specific type of disaster risk in a given location must be quantifiable, with clear calculation methods or graded assessments. If it cannot be measured, how can we verify whether the goal of “reducing disaster risk” has been achieved?

“Disaster resilience” and “disaster prevention and reduction” are not the same conceptually, though this doesn’t mean they cannot be compatible in practice—at the very least, they can facilitate surface-level dialogue. As for donations towards disaster prevention and reduction, they have not increased over the last ten years; they remain very few, with projects being countable on one hand.

The return on investment for disaster prevention and reduction is difficult to measure, as there are few scientifically reliable benchmarks. Moreover, the more successful the effort, the more the situation after a disaster resembles a normal day, making the effect less visible. When benefits are not visible, no one invests. Public opinion easily spots losses that have already occurred, but losses that *could* have happened are rarely calculated seriously.

Ultimately, extreme disasters are low-probability events. If you implement disaster prevention and reduction in 1,000 low-risk communities, it is highly likely that no severe disaster will occur within the effective timeframe of those measures. To improve the effectiveness of investment in prevention and reduction, we must accurately identify high-risk communities—those with a higher probability of suffering severe disaster losses.

◉ Some community development organisations have begun to focus on disaster issues. The Conghua Deep-Rooted Social Work Service Centre found that many irrigation channels in the northern mountains of Conghua had fallen into disrepair, posing a flood risk, and subsequently mobilised villagers to clear silt and repair the channels. Image source: Feng Lian
Regarding community-based disaster prevention and reduction, or the construction of community resilience, are there currently any outstanding examples in China that are worth learning from?
Hao Nan: In terms of the practices being explored by social organisations, schools are doing relatively well; their models are more mature and the outcomes are predictable. At the community level, especially in rural areas, there are successful individual cases, but I have yet to see a model that can be scaled and promoted. It is impossible to scientifically prove that a certain method is effective—that is, that the same method will remain effective if applied to the next village. Currently, many disaster prevention and mitigation activities in rural areas are often completely off the mark, misaligned with the actual risks perceived by the farmers. For example, when creating a community risk map with villagers, I might ask, “If there were an earthquake, which houses in your village would be unsafe?” A villager might reply, “I’ve lived for 80 years and I’ve never seen an earthquake; the biggest risk here is fire—many houses in the nearby hamlets have been burnt down.” I have visited some earthquake-stricken areas where the risks of flooding are actually more frequent and higher. Before the earthquake, community disaster prevention education focused on flooding, but after the earthquake, they only talked about earthquakes and ignored the floods.

Disaster prevention and mitigation often only receive the attention they deserve after a disaster has occurred. However, it is very difficult to teach people how to handle a situation they have never encountered. And the unprecedented disasters that often cause the most severe losses are precisely those historic events that fall outside the local population’s cognition.

Experience in dealing with past disasters is crucial most of the time, but when facing an unprecedented disaster, it can sometimes become an obstacle. This year in the disaster-hit areas of Meizhou and Longyan in Guangdong, we saw that residents on both banks of the river used to move their ground-floor belongings and elderly relatives, who have limited mobility, to the second floor when floods came. But during the extreme floods last June, the water level rose above the second floor…

◉ (Left) June 2025: Heavy rains in the Liujiang River basin in Guangxi led to record-breaking floods in some villages; the water level in the early hours of the 20th was 35cm higher than in 1996. Source: Yang Huiguang; (Right) A Foodthink colleague participated in another post-disaster study tour by Zhuoming in June this year. In Xiaba Town, Wuping County, Longyan City, Fujian, the water had reached the second floor, and flood marks were still visible. Source: Zhou Xuan
The foundation of community work in rural areas is essentially staying long enough to build trust with the locals. The villagers may never have seen what you are talking about, but they are willing to trust you and cooperate with you. But currently, are the organisations providing community services and those handling emergency disaster relief actually two different groups of people?
Hao Nan: Living with the villagers and truly integrating with them—that used to be the working paradigm of international development organisations. In the past, the most thorough community disaster reduction work in China was actually carried out by traditional community development organisations; they recognised that disaster losses were a major factor hindering development, and only then integrated disaster reduction into their projects. But those projects required staff to be stationed in the village for several years. I don’t think many domestic organisations can do that now, nor are funders willing to support it. The biggest problem now is that we no longer have the funds to go into the villages. Who is willing to spend three months eating and drinking with villagers just to teach them a proper evacuation method for disaster prevention? There hasn’t been funding for such projects for several years.

Only a handful of organisations with long-term rural projects can “incidentally” do disaster prevention. You can count such organisations on one hand, and they aren’t necessarily disaster experts. Some organisations just starting community disaster prevention projects ask, “Is there a PPT? Is there a course?” But this isn’t something you can just pick up and use.

Take the act of evacuation, for example; the goal is to move away from risk. But the nature of risk sources in a community—such as landslides, collapses, or heavy precipitation upstream—their attributes, dynamic mechanisms, and the subsequent impact area all require very specific professional expertise to judge. All of this influences the timing of evacuation, the choice of routes, and the formulation of contingency plans. Different types of disasters require different approaches, and the basic conditions of communities vary wildly. The various factors influencing the “awareness, belief, and action” of community residents are even more complex.

Many organisations are now starting to work on community climate adaptation, beginning with an assessment of the community’s meteorological disaster risks. However, everyone reports that this part is difficult to execute. From my observation, it is hard to integrate risk reduction or resilience improvement as a tangible project output.

Governments at all levels now place great importance on life safety. The foundational work for responding to meteorological disasters is being pushed hard, with responsibility passed down through every level. Departments for meteorology, water resources, emergency management, and natural resources are all requiring the grassroots to strictly implement disaster prevention and avoidance measures. For instance, according to the Ministry of Natural Resources, communities must implement “double control” for geological disaster “potential hazard points + risk zones,” and provide simplified guidance cards for disaster prevention and avoidance at hazard points. In theory, rural communities should also establish public welfare posts such as disaster information officers and geological disaster risk monitors.

◉ Simplified guidance card for flash flood disaster prevention. Source: Zhou Xuan

Hao Nan: But implementation is equally difficult. During heavy rain and floods, mudslides and torrents at the source of the disaster often arrive at the same time as the warning, which is different from what is written in most emergency plans. Whether one can develop a method during normal times that actually solves the problem when a disaster strikes becomes the professional dividing line for community disaster prevention projects. Sometimes, community projects can serve to raise awareness, but the actual effect on disaster prevention and mitigation is harder to say.

An organisation once invited us to conduct a disaster risk assessment for a village. The risk background of that village was quite complex, requiring three or four vertical experts to carry out on-site surveys. For example, identifying the front and rear edges of a landslide—as cracks and heaving are precursors to a landslide—estimating the soil structure, understanding how thick and voluminous the potentially sliding soil layer is, which direction it will move, and which households it will affect. The budget for such an assessment was, at most, no more than 5,000 yuan.

Although the money was little, we were willing to participate in such a useful project, but we haven’t encountered another one since.

There is another type of community disaster capacity-building project that is part of a post-disaster support package, which is often a one-off. A friend recently went to Dingri County in Tibet for a community earthquake resistance project; there had been a 6.8 magnitude earthquake earlier that year, and project funding was available. These projects all follow a uniform pattern: they are only carried out where a disaster has already hit, and always within a year. It is essentially providing survivors with a sense of security and psychological comfort. Two years later, the locals no longer want to do it.

Disaster prevention projects, which should belong to the pre-disaster phase, can only be done after the disaster. Relying on the actual occurrence of a disaster to screen for high-risk communities is simply too costly.

On this study tour, you visited Xinglong County in Hebei and the Miyun District of Beijing. What is the grassroots work actually like in these affected areas?
Hao Nan: In Shangshidong Township, Xinglong County, Hebei, the biggest problem in this high-risk township is the lack of manpower. Shangshidong Township covers over 100 square kilometres, but the entire township has a permanent population of only about 1,100 people. In one administrative village that was severely hit, the permanent population is only about 60. The youngest person in the village, chosen as the village chief, is already 55 years old. There is not a single school, kindergarten, or factory in the entire township.

 

◉ Roads near Shanshenmiao Village in Shangshidong Township were once washed away by floods, creating a cliff. Source: Collected from the web by the Zhuoming team
Hao Nan: The village is so aged that we couldn’t even understand the local dialect when we arrived; the young people aren’t home. The young people we did meet were those who had returned during the National Day holiday to help tidy up and deliver supplies; they work in Beijing as entry-level estate agents, courier drivers, or ride-hailing drivers. In a place like this, sending warning notifications via mobile phone is ineffective. You first have to thoroughly understand how the elderly live locally, otherwise, it’s impossible to find a communication channel that is both effective and adapted to the local context.

III. Rocks Rolling Down the Mountain: Louder than the Shouts of Village Officials

Zhuoming has already conducted over ten study tours. You once mentioned that the point of a disaster study tour is essentially to dissect the types and mechanisms of disasters. Specifically regarding this extreme rainfall and flooding, which risks could have been predicted in advance using existing knowledge?
Hao Nan: Flooding alone comes in hundreds of types, and it often occurs alongside various other disasters. In specific disaster scenarios, it is incredibly difficult to provide precise classifications or suggest appropriate countermeasures in advance. Coming from a background in dentistry, I feel our practice in the field of disaster management is still in a ‘trial-and-error’ phase—or rather, we haven’t even mastered the basic anatomy of the different types. To call it ‘medieval’ would be an understatement. Looking back at the extreme rainfall in the Qingshui River basin at the end of July, how did the flood that caused such heavy casualties form? The heavy rain falls, and water surges down the mountains. It progresses step by step: starting as flash floods in the smallest upstream catchments, moving to small and medium rivers, and eventually becoming regional basin floods. The flow velocity, composition, and dynamic mechanisms of the flood are primarily related to the river’s ‘gradient’ (the ratio of the elevation difference to the horizontal distance of a river section, similar to a slope). As the water converges, it carries mud, sand, and stones—each of which requires specific analysis.

Even professionals may struggle to explain these complex dynamic mechanisms. However, in mountainous areas during extreme rainfall, residents must be able to judge the direction of the incoming water—to know whether the threat is a flash flood from the mountains behind their house or a river flood in front. This determines where the chance of survival lies.

Understanding the dynamics of water flow is also critical for rescue operations. In this instance, the Taishitun Elderly Care Centre in Miyun was primarily inundated by rising water; the water rose quickly, but there was a window of one to two hours for people to move to higher ground. Conversely, the village official in Liulimiao Town, Huairou, was swept away by a flash flood in a process that likely lasted only a few seconds; there was simply no opportunity for rescue.

Therefore, disaster prevention and mitigation are far more difficult upstream. It relies on pre-disaster assessments to determine the risk thresholds for rainfall in small basins—knowing exactly how much rain will cause flash floods to destroy where people live. This allows us to establish at what level of rainfall residents must flee. After all, by the time enough rain has actually fallen and the flash flood is imminent, there is no longer enough time to escape. In the mountains, the floods move faster than the red alerts.

In many villages, survivors tell us they heard a sound ‘like thunder’ coming from the mountains. That wasn’t thunder; it was the sound of flash floods and mudslides roaring down the ravines. Beside houses destroyed by landslides and mudflows, there is a powerful wind and a surging blast of air. These sounds are so deafening that, when the disaster strikes, they completely drown out the shouts of village officials calling for evacuation.

This is why so many grassroots officials have been killed or injured in recent years—while others flee, they head towards the danger. I specifically went to the site to reconstruct the sequence of events where a village party secretary and his companion were swept away—how they stepped out of the village committee office, were knocked down by a torrent of mud and water, and were carried step by step into the river…

◉ During this year’s Miyun floods, the Sohu Farm on the banks of the Qingshui River was ruthlessly swallowed up. Foodthink’s article documents the process of farm employees being swept away by the floods and their narrow escape. Image source: Sohu Farm
So, how do we assess in advance how much rainfall a small mountain basin can sustain, or in other words, what its ‘precipitation threshold’ is?
Hao Nan: To determine precipitation thresholds and assess disaster risk, one must accurately simulate how much rainfall within a specific small catchment will trigger floods powerful enough to wash away gully beds and raise downstream water levels. This requires integrating data on topography, vegetation, soil, lithology, catchment area, and slope to calculate the rain-collection area. This must then be combined with precipitation levels and land surface conditions to calculate the surface runoff conversion rate—this falls squarely within the professional remit of water resources departments. However, based on their functional division, the Ministry of Water Resources is more concerned with how to regulate and store floodwaters after they have been produced, accumulated, and flowed, and how to mitigate risks within existing downstream hydraulic facilities. How a community should respond—and specifically what disasters are caused by flash floods at the furthest upstream reaches—falls into their blind spot and outside their official duties.

In reality, the Ministry of Natural Resources is responsible for managing geological disasters. In their definitions, flash floods are often categorised under the comprehensive management of small mountain basins and merged with geological hazards.

When we arrived on-site, we found that in some townships, the Water Affairs Bureau was still conducting door-to-door disaster risk assessments. In my view, according to their routine duties, they can only assess areas along riverbanks. Whether this covers flash floods and geological hazards is a question.

Those with the capacity to calculate floods do not manage small catchments; they mainly manage river channels. Meanwhile, those who manage small catchment disasters are not proficient in hydrological and hydrodynamic modelling. There are clearly silos here that need to be broken down.

You mentioned that floods travel faster than red alerts. Setting aside scientific calculations and disaster mechanisms, the issue that concerns the public most is: when should they evacuate? What knowledge or tools can help us make this judgement, and what experiences can be summarised from local areas?
Hao Nan: Firstly, during the extreme rainfall in the Qingshui River basin, the key point was that the people responsible for the work did not sleep. Getting emergency notices at two or three in the morning to evacuate the masses is not easy for village officials in their fifties or sixties. They managed, at the very least, to avoid greater casualties; this is the experience that should be summarised.
*Editor’s note: In the early hours of 29 July, nine villages under the jurisdiction of Shangshidong Township lost contact with the township government one after another. Due to flash floods and debris flows triggered by torrential rain, electricity, communications, and roads across all nine administrative villages were severed, turning them into isolated islands. Cao Zuofeng, Party Secretary of Shangshidong Township, once trekked 37.9 kilometres on foot to confirm the safety of villagers in each village.

◉Mipu Village in Shangshidong Township is located within a narrow mountain valley and suffered severe debris flows and flash floods. On 4 October, the roads leading to Mipu Village were completely washed away or collapsed; vehicles had to drive through riverbeds carved out by floods, with the original roadbeds now towering above them. Farmland previously in the riverbed is now entirely covered by boulders. Image source: Xie Yijing

Hao Nan: But when we return to the science of how to judge the timing of evacuation, the problem arises. In the worst-hit areas of this flood, evacuation decisions were based on flood water level standards for 5, 10, or 50-year return periods, in accordance with the flood control response plans of water resources departments.

However, the frequency of a flood (e.g., once in 50 years) is an engineering design standard based on probability statistics. Using this as a standard for personnel evacuation is often only effective for the banks of downstream river channels; it may not be a useful reference for upstream areas. Evacuations for river floods in Xinglong County were relatively successful this time because water accumulation takes time, usually giving residents a window of several hours to escape. The casualties were primarily caused by flash floods and debris flows, which occur much earlier and closer to the time of extreme precipitation. If you evacuate using the methods designed for river floods, it is too late.

The same issue applies to the short-term heavy rain warnings from the meteorological departments—red alerts for torrential rain are generally issued at the county level, indicating 100mm of rain or more in 3 hours, or 50mm or more in 1 hour. However, these are hardly actionable for evacuations in specific townships or streets. Again, they are more effective for downstream river flooding.

Based on the overall precipitation, Xinglong County issued a red alert after 2 a.m. However, between 1 a.m. and 2 a.m., local precipitation in Yingnanyu Village, Shangshidong Township, had already reached 91mm. In Zizigou, further upstream from Yingnanyu, flash floods began ravaging the area around 1:30 a.m.—the critical value I mentioned earlier, the small catchment precipitation threshold, had been reached long before the red alert.

Therefore, the decision of when to evacuate at the grassroots level is still largely decided based on the actual situation on the ground. Currently, the professional strength and resources that the front line of disaster prevention and mitigation can rely on are still quite scarce.

So, do you believe that evacuation points should be calculated locally, based on the precipitation thresholds of each catchment?
Hao Nan: Yes. As soon as the precipitation in the upper reaches of a small catchment approaches the disaster threshold, downstream personnel must be notified to evacuate immediately. There is no need to wait for broader rainfall statistics or warning notices. Some grassroots areas have already begun calculating small catchment precipitation thresholds. In mid-July this year, we visited a village that had suffered significant casualties from a geological disaster two years ago. Based on measurements from a flash flood rain gauge, as soon as precipitation reaches the threshold, the village’s loudspeakers emit a high-pitched alarm to prompt villagers to evacuate. It rained the night before we arrived, and the villagers evacuated overnight. By the time we reached the village, it was almost empty. This has become their norm during the flood season. In other more complex scenarios, it is almost impossible—even from a professional perspective—to precisely calculate the time, location, and scale of a disaster in advance, but local residents should at least be aware of the possibility of compound risks.

For example, in Yangjiatai Village in Liudaohe Town, Xinglong County, which was severely hit, flash floods and debris flows erupted from two directions almost simultaneously, completely blocking the escape routes… this was the area with the highest number of geological disaster casualties.

The red alert for Xinglong County was issued after 2 a.m. In the small catchment where Yangjiatai Village is located, the torrential rain actually only began after 3 a.m. By four or five o’clock, the extremity of the rainfall broke the soil-rock balance at the mountain peaks, and flash floods and debris flows erupted simultaneously from several branch gullies at high altitudes upstream. A large portion converged in front of groups four and five of Yangjiatai Village, first destroying several houses and courtyard walls at the bottom of the gully; a smaller portion converged into the flash flood gully behind group four, from where it subsequently levelled most of the houses and fields in that section.

◉Shangshidong Township under reconstruction. Image source: Hao Nan

IV. Treating “Tooth Decay”: The Need for Both Research and Community Doctors

Hao Nan: Overall, in terms of responding to meteorological disasters, China is still at the forefront of the world, and there is less and less experience to be borrowed internationally. Most of our regions have a monsoon climate, making China one of the countries with the most meteorological disasters, and the effects of the climate crisis were felt here earliest and most profoundly. The topography is diverse, and all types of disasters are represented. Mountainous areas and river valleys are densely populated. Only a few other countries possess all these characteristics. Currently, the geological structure of all regions in China, every subdivided type of disaster, and the dynamic mechanisms of every stage of flood disasters have actually been studied very clearly. However, in practical application, the upstream and downstream of academia are not connected.

From a social perspective, if you do not know how a disaster happens or understand its “pathogenesis”, you cannot effectively prevent or “treat” it. It is as if someone has researched the causes and treatments of “tooth decay”, but no one is doing “public health” to popularise and intervene in people’s health behaviours, nor are there “community doctors” to help specific patients with prescriptions. Consequently, the problem of “decayed teeth” cannot be solved.

Report Recommendation

A report recently released by Foodthink, “Research on the Action Path of Rural Social Organisations in Response to Climate Change”, detailed cases of how Zhuo Ming’s team responded to natural disasters and acted as an “information hub”. Click the link to download the full report.

Foodthink Author
Pei Dan
A writer back on her true path, focusing on climate change, the ecological environment, and the individuals affected by these transitions.

 

 

 

 

Editor: Ling Yu