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位于俄罗斯堪察加半岛太平洋沿岸的火山群克拉谢宁尼科夫(Krasheninnikov),在沉寂了近五个世纪之后于 2025 年重新喷发。美印合成的 NASA-ISRO 合成孔径雷达卫星(NISAR)从 747 公里高的轨道上,以每 12 天两次的重访频率,持续记录了熔岩流从火山口喷涌、填充破火山口、最终向外扩展成扇形的完整过程。康奈尔大学地球物理学家、NISAR 科学团队成员 Matthew Pritchard 将 17 帧雷达影像串联成延时视频,直观展示了这座苏醒火山的地貌演变,也验证了 NISAR 在自然灾害监测领域的实用价值。
这次喷发的诱因耐人寻味。2025 年 7 月 30 日,附近海域发生 8.8 级强震,数天之后,克拉谢宁尼科夫火山便开始喷发——这是该火山自约 1550 年以来的首次活动。地震与火山活动的关联机制仍有待研究,但 NISAR 恰好赶上了这一罕见的地质事件:2025 年 12 月 25 日,刚刚完成发射后测试、转入业务运行状态的 NISAR 便拍摄到首批影像。此后卫星以固定轨道周期反复掠过同一地点,升轨与降轨各成像一次,积累了连续的观测序列。
微波成像:从模糊到聚焦的遥感革命
NISAR 的成像能力源自合成孔径雷达(SAR)技术,这一处理方法由 NASA 位于南加州的喷气推进实验室(JPL)率先用于对地观测。卫星在轨运行时,雷达每秒向地面发射数千个微波脉冲并接收回波信号,每一组回波都承载着地表特性的信息。SAR 处理将同一区域的多幅影像合成,如同透镜将模糊物体聚焦成清晰图像。
在此次火山延时影像中,每个像素对应地表约 10 米×10 米的方形区域,大约是半个网球场的大小。由于微波在熔岩表面的反射比周围的积雪或裸地更为明亮,熔岩流在影像中呈现更亮的色调。视频清晰显示熔岩首先填充内部较小的破火山口,随后溢出到更宽的外侧火山口,最终向东部扩展成扇形,同时西北方向还存在一条疑似在 NISAR 首次成像之前形成的早期熔岩流。
【关键数据】
- 轨道高度: 747 公里
- 重访频率: 每 12 天两次(升轨、降轨各一次)
- 影像分辨率: 10 米×10 米/像素
- 火山休眠时长: 近 500 年(自约 1550 年)
- 延时影像帧数: 17 帧(2025 年 12 月至 2026 年 8 月中旬)

双频段设计与全球火山监测盲区补全
NISAR 是首个搭载两部雷达仪器的自由飞行航天器:L 频段与 S 频段系统。两个频段波长不同、功能互补——波长更长的 L 频段可以穿透树冠直接成像地面,而 S 频段则可根据叶片尺寸获取冠层信息。这种双频配置使 NISAR 能够在植被覆盖区域同时获取地表与植被信息,在森林生物量估算、地表形变监测等应用中具备独特优势。其 L 频段数据产品已在位于费尔班克斯的阿拉斯加卫星设施分布式活性档案中心开放分发。
对火山学界而言,NISAR 带来的改变更为直接。堪察加半岛虽拥有数十座火山,但因喷发频繁,多数火山配有地面监测设备,而长期休眠的克拉谢宁尼科夫恰恰处于监测盲区——L 频段雷达能够捕捉到它,本身便印证了 NISAR 对全球陆地表面近乎无死角的覆盖能力。Pritchard 回忆,二十多年前他攻读博士学位研究堪察加火山时,卫星重访频率低、影像分辨率有限,可用数据极为稀缺。如今全球约 1300 座海拔以上的活火山几乎全部纳入观测范围,影像分辨率精细到米级,且可通过云端便捷获取。
"我们正以前所未有的视角观察世界各地的火山,"Pritchard 如此评价。延时影像所展示的不只是单一火山的动态,更是一套可复制到全球灾害监测的观测范式——高分辨率、固定周期、双向成像的组合,使科研人员乃至应急响应机构都能及时掌握自然灾害的演化进程。
对地观测格局的潜在变量
从产业视角看,NISAR 的稳定运行进一步压缩了全球灾害监测的观测盲区。随着其数据通过云端向全球科研与应急机构开放,火山、地震、洪水、冰川消融等领域的响应时效有望显著提升。对通信与遥感产业而言,双频 SAR 的业务化验证也为后续商业 SAR 卫星星座的技术选型提供了重要参照。在自然灾害日益受关注的当下,这类近全球覆盖、米级分辨率的天基监测能力,正在成为空间基础设施中不可替代的一环。
出处:US-India Satellite Captures Time-lapse Video of Volcanic Eruption
英文原文
In this animation, frames of NISAR data from December 2025 to August 2026 show the spread of lava from the northern crater of Krasheninnikov, a volcano pair on Russia’s Kamchatka Peninsula. In the image, the lava field appears brighter in the foreground than the surrounding surfaces. Credit: NASA’s Scientific Visualization Studio Like tendrils on a vine, lava spreads out from the northern crater of Krasheninnikov, a volcano pair on the Pacific coast of Russia’s Kamchatka Peninsula. On July 30, 2025, an 8.8-magnitude earthquake had struck in the nearby ocean, apparently jolting one of the two volcanoes awake. A few days later, for the first time in nearly five centuries, Krasheninnikov started erupting. Since that day, the northern volcano has been spilling a steady, eastward-flowing field of molten rock and debris, and the NASA-ISRO Synthetic Aperture Radar (NISAR) mission has been tracking the changes in the landscape. From its vantage point 464 miles (747 kilometers) above the surface, NISAR captured an image of Krasheninnikov on Dec. 25, 2025, just as the Earth-observing satellite was finishing post-launch checks and becoming operational. Twice every 12 days since — once as the satellite passed south to north, and again as it passed north to south — NISAR has returned to the same spot in orbit and taken detailed radar snapshots. Researchers put 17 of the frames captured through mid-August into sequence, forming a time-lapse video that shows lava filling a smaller, inner caldera, then overflowing into a wider crater before widening into a fan. The animation highlights how NISAR’s observations can monitor the development of natural hazards, both for science and potentially for emergency response. Though remote, many of Kamchatka’s dozens of volcanoes are closely monitored with ground instruments because they erupt frequently. Not so with Krasheninnikov, which has been quiet since about the year 1550. That NISAR’s L-band radar observed it at all speaks to the satellite’s near-global coverage of the planet’s land surface at resolutions in the dozens of feet; that it captured the erupting volcano over time shows the precision and reliability of its measurements. “The consistency is crucial. Twice every 12 days, acquiring in this high-resolution mode and in two observation directions, this shows the promise of NISAR to closely monitor natural hazards,” said Matthew Pritchard, a member of the NISAR science team and geophysicist at Cornell University who analyzed the data used to create the animation. Images from microwaves The detail in a single NISAR image results from the use of synthetic aperture radar, or SAR, a specialized processing technique pioneered by NASA’s Jet Propulsion Laboratory in Southern California for Earth observation from space. As the satellite orbits, the radar sends thousands of microwave pulses per second to Earth and receives the return signals, each of which is effectively a snapshot in time that contains information about the properties and characteristics of the surface below. The SAR processing combines the many images of the same area, sharpening the view just as a lens brings a blurry object into focus. Each pixel in the individual frames of the Krasheninnikov time-lapse represents about a 30-foot-by-30-foot (10-meter-by-10-meter) square on the surface — about half the size of a tennis court. Lava shows up lighter in the images due to the way that microwaves reflect more brightly compared with the surrounding surface, which, depending on the time of year, is either snow or bare ground. In addition to the lava field growing to the east, the video shows another flow to the northwest, one that likely formed before NISAR captured the first NISAR image. When Pritchard was doing his doctoral research on Kamchatka volcanoes more than 20 years ago, analysis-ready radar data was difficult to come by, both because satellites didn’t revisit as often and the resolution of the images was relatively low. Now in addition to getting frequent and comprehensive coverage of virtually all the planet’s roughly 1,300 active, above-sea-level volcanoes, the images are sharp down to the several-meter scale and are easily accessible via the cloud. “We’re seeing volcanoes around the world that we’ve never really had eyes on like this before,” said Pritchard. The NISAR satellite is the first free-flying space mission to feature two radar instruments: an L-band system and an S-band system. The systems are complementary due to their differing wavelengths. For example, the longer-wave L-band can pass through tree canopies, imaging the ground beneath. Meanwhile, depending on leaf sizes, S-band can collect observations of those canopies. The data products from the NISAR mission’s L-band radar are available at the Alaska Satellite Facility Distributed Active Archive Center in Fairbanks, which hosts and distributes all NASA synthetic aperture radar data. More about NISAR Managed by Caltech for NASA, JP