Hypothermia Risk Assessor失温风险评估器
Temperature, wind, wet clothes and fatigue — risk band, symptom staging and field rewarming steps. 气温、风、湿衣与疲劳——风险分级、症状分期与野外复温步骤。
How the risk assessment works
Hypothermia is a heat-budget problem: your body loses warmth faster than it makes it. The assessor combines a physical cold component — the National Weather Service wind-chill temperature when it applies — with the four factors that dominate real backcountry cases: wetness, fatigue, exposure and injury.
The NWS wind-chill formula describes convective cooling on exposed skin from air temperature and wind speed. Its valid range is air temperature at or below 50 °F (10 °C) with wind above 3 mph; outside that range the tool falls back to plain air-temperature bands, because wind chill says nothing about rain, sweat or immersion. Crucially, most hypothermia incidents happen above freezing, in 0–10 °C rain and wind, when hikers underestimate the chill because the thermometer looks mild.
Why wetness and fatigue dominate
Water conducts heat roughly twenty-five times faster than air, so soaked clothing turns an uncomfortable afternoon into an emergency; sweat from overdressing works as well as rain. Exhaustion removes the last defenses: shivering itself is hard muscular work that burns calories and glycogen, and a tired, hungry hiker cannot generate enough heat to catch up. River immersion compresses the whole timeline into minutes.
Mild versus severe — the staging that matters
Mild hypothermia, a core temperature of roughly 32–35 °C, is a field-reversible emergency: vigorous shivering, fumbling fingers, grumpy apathy and slurred speech. Below 32 °C the picture changes — shivering stops, muscles go rigid, pulse slows and confusion deepens into drowsiness. That transition is the call-now line. Treatment is a complete hypothermia wrap: shelter, dry layers, insulation under and over the body, gentle handling, a vapor barrier such as a bivvy, and skin-to-skin contact in a sleeping bag. A sugary warm drink helps only someone fully awake and swallowing. Avoid the famous myths: no alcohol, no rubbing, no direct heat, no forced walking — and in rescue medicine, no one is dead until they are warm and dead, so CPR continues through evacuation.
风险评估是怎么算的
失温本质上是热量收支问题:身体失热速度超过产热速度。本评估器把物理寒冷分量——适用时采用美国国家气象局(NWS)风寒温度——与真实野外失温案例中最关键的四个因素合并:潮湿、疲劳、暴露与受伤。
NWS 风寒公式描述气温与风对裸露皮肤的对流冷却,适用范围是气温不高于 10 °C(50 °F)、风速大于 3 mph;超出范围时工具改用纯气温区间,因为风寒无法反映降雨、出汗或落水。必须强调:大多数失温发生在冰点以上——0–10 °C 的风雨中,徒步者看到温度计不算低就放松了警惕。
为什么潮湿和疲劳最关键
水的导热速度约为空气的 25 倍,湿透的衣物能让一个难受的下午迅速变成急症;穿太多闷出的汗和雨水效果相同。精疲力尽则撤掉了最后防线:颤抖本身是高强度肌肉劳动,消耗热量与糖原,又累又饿的人无法再产热追平失热。落水则会把整个过程压缩到几分钟内。
轻度与重度——最关键的分期
轻度失温(核心温度约 32–35 °C)在野外仍可逆转:剧烈颤抖、手指不灵活、冷漠易怒、说话含糊。低于 32 °C 时情况改变——颤抖停止、肌肉僵硬、脉搏变慢、意识混乱加深为嗜睡。这个转折就是立即求救线。处置是完整的失温包裹:遮蔽、干衣、身下与身上都隔热、动作轻柔、外层用应急睡袋等蒸汽阻隔物,并在睡袋内皮肤贴皮肤复温。含糖热饮只给完全清醒、能吞咽的人。务必避开著名误区:不饮酒、不搓揉、不直接热敷、不强迫行走;在救援医学中“未复温,不算死”,心肺复苏应在转运中持续进行。