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Wednesday, September 17, 2025

Himalayas: monsoon reached Tibetan Plateau- unprecedented hydro meteorological event, Paul Beckwith report at Heating Planet blog

Usually I use a quote from the transcript for first paragraph of blog posts. But everything Paul Beckwith says in this video is important. For example  “Atmospheric rivers and changes in jet streams seemed to drive the monsoon moisture to higher and higher levels. In fact, parts of it seemed to cross the Himalayas and reach the Tibetan plateau just a few weeks ago. And if this is the case, it's unprecedented.” Beckwith is a climate system science educator on abrupt climate change. WATCH: Unprecedented: Monsoon Winds Breached Himalayan Mountains Bringing Rain and Snow to Tibetan Plateau [transcript below]


Part 2 Himalayan flood videos 

TRANSCRIPT by AI: 

"Hello everybody. 0:05 My name is Beckwith, 0:07 Paul Beckwith. 0:09 About a week ago, there were a number of 0:11 different news articles from various 0:13 meteorologists in different countries 0:16 asking the question, did the southwest 0:19 monsoon moisture actually cross the 0:22 Himalayas and reach the Tibetan plateau 0:25 um just uh you know, a week or two ago? 0:29 So the monsoon in India has been ex very 0:32 very powerful this year. Very intense 0:35 started early still ongoing. Um and it 0:40 normally is at lower levels in the in 0:44 the atmosphere. So you know it's 0:46 normally between about 1,600700 0:49 m up to 2,000 mters maybe. But this year 0:53 there were some exceptional weather 0:55 conditions, you know, with jet streams 0:58 and atmospheric rivers and things that 1:00 seemed to drive the monsoon 1:04 moisture to higher and higher levels. 1:06 And in fact, parts of it seemed to cross 1:09 the Himalayas and reach the, you know, 1:12 parts of the Tibetan plateau just a few 1:14 weeks ago. And if this is the case, it's 1:16 unprecedented. 1:18 So, I want to look at some of the um I 1:22 did a little bit of investigation and 1:24 I'll I wanted to uh let you know some of 1:26 the things that I've come up with. 1:30 Okay. So, yes, the monsoon winds did 1:33 seem to cross the mountains into Tibet 1:36 in early September 2025. 1:39 So this is from what we can see an 1:42 unprecedented event and it's being 1:45 attributed to shifting climate dynamics 1:48 and it's being confirmed by multiple 1:50 weather and climate sources. Okay, so 1:53 that's the first thing. 1:56 Second thing, climate scientists and 1:58 glaciologists analyzing satellite data 2:02 have confirmed that the southwest 2:04 monsoon. So it's from the southwest 2:07 moving up towards the northeast. It's 2:10 traditionally blocked by the Himalayas, 2:13 right? The mountains are just too high. 2:15 It blocks it, creates a barrier. But 2:18 that barrier seemed to be breached. So 2:21 moisture was carried up to very high 2:23 altitude into Tibet during the first 2:26 week of September of this year. This is 2:29 the first recorded instance where the 2:32 monsoons moisture penetrated into Tibet 2:36 apparently. Um needs more investigation 2:39 to see if that's actually true. Um, but 2:42 it's very raw, very dry in the 2:44 mountains, high in the mountains because 2:46 the moisture precipitates out before it 2:48 reaches the high elevations. 2:51 So, this event that happened just a 2:53 couple weeks ago, it's been called 2:55 extraordinary, potentially significant 2:58 for future regional water security and 3:00 weather patterns. So, what actually 3:03 happened? Um, apparently there was a 3:06 series of so-called western disturbances 3:10 that interacted with the monsoon winds 3:13 and that drove the moist air to very 3:15 very high altitudes, allowed moisture to 3:18 cross the the mountains into Tibet. And 3:23 most of the information we have on this 3:25 event happening is from satellite 3:27 images. They show a clear migration of 3:30 the moisture from over Hamashial 3:33 Pradesh, 3:35 Utaric Kahand and Leiddaka, into the 3:39 Tibetan plateau. 3:41 And there's a there's a region called 3:43 Zanscar, Zan S. 3:47 It's close to the divide of the 3:50 mountains. They got over 100 millimeters 3:52 of rain and even unseasonable snowfall 3:56 during this event just from a couple 3:58 weeks ago. Okay. So, this event's viewed 4:01 as a direct consequence of climate 4:03 change affecting South Asian weather 4:06 systems which there's been an increase 4:09 in variability and intensity of these of 4:12 hydro meteorological events, water, 4:15 weather events. 4:18 local populations in Tibet and 4:20 surrounding regions saw unusual 4:22 precipitation levels and humidity. 4:24 Right? Normally it's very typically very 4:26 very dry in September, but they didn't 4:29 get that this year. So this is a very 4:32 significant and important anomaly 4:36 um which is going to need a lot of 4:38 study. So it's basically a convergence 4:41 of unusual factors, unusual weather 4:44 factors that are not aren't normally 4:46 seen in the region. So the key thing is 4:48 first of all the monsoon's been pretty 4:51 intense in India. You know very very 4:54 intense long duration huge amounts of 4:56 rainfall. I'll talk about some of the 4:58 details to follow in this video but the 5:02 there's been a record number of these 5:04 so-called western disturbances. There's 5:06 been 19 western disturbances during the 5:09 southwest monsoon season. Normally 5:12 there's about four to six. So we've got 5:14 at least uh you know maybe five three to 5:17 five times more uh disturbances 5:21 um than than normal. So the dynamics 5:25 there's powerful dynamics going on in 5:27 the atmosphere above India and these are 5:30 directly affected 5:33 um and interact directly with the 5:35 monsoon winds the moist monsoon winds. 5:38 So the monsoon winds have been very 5:40 strong and there's been very intense 5:43 uplift. So these disturbances 5:46 being dragged along by the monsoon that 5:49 increases the vertical transport of air 5:51 when they're pushed against the 5:52 mountains. So the moisture laden winds 5:56 went to altitudes. It just says you know 5:59 over 2,000 meters. But in order to reach 6:02 um you know through further in it would 6:04 have to go through valleys mountain 6:06 valleys and things and reach you know 6:08 3,000 4,000 plus meters in order to in 6:12 order to be seen over the regions where 6:14 this where the snow and precipitation 6:16 occurred. The normal monsoon height is 6:19 around 1,600 to700 meters. So we went 6:23 much higher than that and we've breached 6:25 the Himalayan barrier. 6:28 the there's been a lot of atmospheric 6:31 heating and expansion temperatures well 6:33 above norms in India much more 6:37 convective uplift bringing things to 6:39 higher bringing moisture to higher 6:40 altitudes the collision of the western 6:43 disturbances with the strong monsunal 6:46 advection that's horizontal movement of 6:48 air led to warming uplift and expansion 6:51 of the moist air so it created clouds 6:54 and moisture which spilled over over 6:56 gaps in the mountains As seen from 6:58 satellite um monitoring, 7:02 there's a possible involvement of 7:04 atmospheric rivers and the subtropical 7:07 jet in this region. So that needs to be 7:10 looked at. Like I say, this is this 7:11 event just happened, you know, last 7:14 week. Basically, 7:16 some climate scientists have suggested 7:18 atmospheric rivers or shifts in the 7:20 subtropical jetream to transport 7:22 moisture beyond the Himalayas. So that 7:25 needs to be looked at. of course in more 7:27 detail. I'll do a whole separate video 7:30 soon on the phenomena of atmospheric 7:33 rivers and how they're changing under 7:35 climate change. So, climate change 7:37 underlies all of these things. It 7:40 contributed to more frequent and intense 7:42 disturbances, these so-called western 7:44 disturbances. 7:46 The it it's amplified the energy in the 7:48 monsoon. There's more unpredictably, 7:51 more variability, so rare events become 7:53 more possible. So it's a synergy of 7:56 different meteorological events. So 7:59 let's have a look at what um some of the 8:02 articles have been saying on this 8:05 particular phenomena. 8:09 Okay. So first of all 8:13 this this was um an article um from a 8:17 month or so ago. South Asian monsoon 8:20 2025 wetter hotter and more 8:22 unpredictable. This is global from 8:24 global climate risks. 8:27 Okay. So they've had an intensified 8:29 summer monsoon temperatures forecasted 8:32 up to two Celsius above normal above 8:34 average rainfall across India, Nepal, 8:37 Tibet and neighboring regions. 8:40 Um 8:43 and you know of course most of the 8:45 flooding in South Asia about 3/4 of it 8:49 occurs during summer monsoons. 8:52 Um so there are there are mortalities 8:55 from this. So June to August Pakistan 8:57 had deadly floods, intense monsoon 8:59 rains, 260 people lost their lives. In 9:03 North India, heavy monsoon rains 9:05 triggered deaths from cloud bursts, 9:07 flash floods, landslides. 9:10 The state reported 25 cloud bursts and 9:12 over 40 flood events. So like the the 9:15 sky just falls on you basically all the 9:17 moisture in the sky. Um, nep Nepal uh 31 9:23 deaths, 151 injuries, 682 monsoon 9:26 related events. So the weather is just 9:28 gone haywire there plus two Celsius 9:32 seasonal anomalies in temperature, above 9:34 average rainfall. 9:36 The agriculture and water systems in 9:38 South Asia support nearly two billion 9:40 people. So there's more vulnerability 9:42 with increased variability. 9:45 The monsoon circulation is trending to 9:48 becoming weaker even though rainfall is 9:50 increasing. This contradiction is caused 9:53 by global warming. It increases heat and 9:55 moisture in the atmosphere. It can 9:56 reduce vertical air movement. It says 9:58 here the weather whiplashing is a 10:02 variation within a single monsoon season 10:05 like the switching between wet and dry 10:07 and wet and dry. It's hard to predict 10:09 these things. Enso's playing a role. 10:12 They talk about the polar warming, 10:15 disrupting the jet streams, affecting 10:17 the um causing more erratic behavior. 10:21 Okay, so this um so this monsoon's been 10:24 pretty intense. 10:26 Um this is an update on uh the monsoon 10:30 rains uh from just um the end of August. 10:34 Um climate change definitely intensified 10:38 has intensified India's rains. So the 10:41 monsoon this year, it was unusually 10:43 severe. It arrived earlier than 10:46 expected, caused widespread damage. 10:49 Climate change has intensified it. 10:51 There's been multiple so-called western 10:53 disturbances that contribute to extreme 10:55 weather events. 10:58 So so these things uh it arrived um 14 11:03 to 18 days earlier than forecast. it 11:06 pummeled collect you know different 11:08 areas as it moved across India 11:11 um flash floods really high flooding 11:15 erratic behavior the monsoon uh it's it 11:19 says it's it by by end of August it had 11:22 already that the region had already seen 11:25 15 western disturbances right and that 11:28 number increased as I mentioned in the 11:30 introduction 11:33 and uh flash flooding and and and and 11:35 and so on. So very intense monsoons 11:39 being going on. 11:41 Um this is the government of India um 11:44 earth system science organization. So 11:47 what they have to say this is a press 11:49 release from just a few days ago 11:52 September 11 2025 11:54 about different um behaviors of the 11:58 monsoon. But this is this is just over 12:00 India. Okay. It talks about north uh 12:04 north India, northwest India. Um it 12:08 talks about all regions of of India. So 12:11 different um rainfall amounts and 12:14 departures and so on. So there's a lot 12:16 of regional differences. Some areas, you 12:19 know, like 12:21 are only getting half the rainfall. 12:23 Other areas are getting almost well 40% 12:26 more in other regions. Okay? So there's 12:29 a lot of variability. um they give 12:31 forecasts and so on. So there's there 12:34 but it doesn't talk really about um the 12:37 about the monsoon crossing the 12:38 Himalayas. So this is uh one of the 12:41 articles. So I I have a whole bunch of 12:42 different articles. I'm just going to 12:44 show you some stuff. Um so monsoon 12:47 breaches Himalayas, moisture reaches 12:49 Tibet. Um so so southwest monsoon winds 12:54 cross the Himalayas carried moisture 12:56 into Tibet. 12:57 It's normally blocked by the mountain 12:59 barrier. 13:01 Right. But it uh Tibet's largely dry. So 13:05 when it's blocked by the mountain 13:06 barrier, the rain has the the clouds 13:08 have nowhere to go. I mean, they deposit 13:10 their rain in India, Nepal, and Bhutan 13:13 while leaving the area, but Tibet's 13:15 largely dry, but it's mostly there's not 13:18 a lot of weather stations up in Tibet. 13:20 satellite images show the moisture 13:22 drifting um into into the Tibetan 13:25 plateau and it's a very rare occurrence 13:28 possibly unprecedented. It's been 13:30 related to global warming increased 13:32 weather disturbances. Okay, so it's an 13:35 extraordinarily 13:37 extraordinary and potentially 13:38 significant for South Asian Asia's 13:41 weather and ecosystem. So there's so 13:44 let's look at the region where we are. 13:46 This is the region um Zanscar 13:50 is right this region right here. Okay. 13:53 Elevation actually look at the elevation 13:56 down here 3530 m. Um but but here's 14:02 where where where we are. So the the 14:06 moisture has come right in and made it 14:08 up to there probably through different 14:12 valleys, you know, different valleys and 14:14 roots, but it still got across, you 14:16 know, this is uh 3,700 m. You know, 14:21 there's some air 4,000 m. Okay, it still 14:24 has to go extremely high in order to get 14:27 up to this region. I'm going to back off 14:29 a bit and you can see, you know, India 14:32 here. 14:33 um you know so this is the uh so so 14:38 the winds are from the southwest moving 14:41 to the northeast and and there was so 14:44 much moisture from the so-called western 14:46 disturbances added to the the monsoon 14:50 vected that moisture up it reached the 14:52 um mountains and got uplifted it was 14:55 already at higher than normal levels 14:57 anyway some of it made it up into here 14:59 100 millimeters of rain and snow in this 15:01 region so the barrier area normally it's 15:04 very very dry up here and you get 15:06 tremendous rainfall here. So the 15:08 contrast is enormous because of the 15:10 topography 15:12 but you know the so-called him Himalayan 15:15 divide uh was breached because of the 15:18 intensity of these uh of of of the the 15:22 moisture and it probably atmospheric 15:24 rivers were associated andor the jetream 15:27 but I'll have to talk about those those 15:29 those in in a future video. Um, this is 15:33 Earth Null School. You can kind of look 15:34 at the uh, you know, what's going on 15:36 with the winds and you can, you know, 15:39 you can what's going on now, you know, 15:42 and you can see, you can go back to the 15:44 dates. Um, this is September 16. You can 15:47 go back to the dates. You can scroll 15:48 back a day, you know, a you can scroll 15:51 back in time or just go here and set the 15:54 date. So, this is like September 1st 15:58 conditions on September 1st. If you you 16:01 can advance forward and we're talking 16:04 about the breaching up these winds up 16:06 here. Um this is a this is ground level 16:09 winds. Um you can go up to various uh 16:14 you know you can look at what the jet 16:15 streams are doing back in this time for 16:17 example 16:19 and see uh you can see you know this you 16:23 I I think you could see you know we're 16:26 up here. Is it is it this moisture being 16:28 carried up by up this by here? This is 16:31 September 3rd. 16:34 Maybe this shifts down over time. 16:37 Sorry, I'm hitting the wrong button. 16:40 Uh 16:42 September 4th, 16:44 September 5th, 16:48 you know, maybe I'm guessing it probably 16:50 happened about here. 16:53 I don't know. I mean, is this is this 16:54 part of the phenomena? Anyway, you can 16:56 play around with the Earth's null school 16:58 and have a look some other articles. 17:01 Monsoon crosses the Himalayas into Tibet 17:04 are bigger disasters ahead. 17:07 Okay, so there was a lot of um noise 17:10 about this about a week ago. Then it 17:12 dropped off the map being replaced by 17:14 other things. But basically satellite 17:16 images, field studies point to global 17:19 warming and an unusual rise in western 17:21 disturbances. So a lot more than normal 17:23 as I mentioned. 17:25 Um and then when you combine that with 17:27 the advection the the the winds uh 17:31 horizontal winds due from the monsoon 17:34 carrying it to the barrier in the 17:36 Himalayas. It has nowhere to go but up 17:38 or or to split across because normally 17:41 the towering wall of the Himalayas 17:43 blocks these winds. They strike the 17:45 mountain ranges, unload rain across 17:47 India, Nepal and Bhutan and leave Tibet 17:49 largely dry. But in the first week of 17:52 September 2025, satellites captured 17:54 moisture drifting up into the Tibetan 17:57 plateau, breaching the Himalayan divide. 18:00 Okay, so that's so you know, and there's 18:03 people there, you know, the images are 18:04 clear, the satellite images are clear. 18:06 The moisture breached the Himalayan 18:08 bearer and traveled north into Tibet. 18:10 It's unusual because the Himalayans 18:12 usually hold the line. Why did this 18:15 happen? Um they mentioned the unusually 18:18 high number of western disturbances in 18:20 this monsoon season. 19 disturbances 18:24 have been recorded. Five each in June, 18:26 July and August and three more in early 18:29 September. 18:30 These weather systems are usually winter 18:34 phenomena. They bring rain and snow to 18:36 North India and the Himalayas in the 18:38 colder months. But this year they 18:40 happened earlier. They collided with the 18:43 monsoons moist currents which is very 18:45 unusual. and that's pushed them further 18:46 north to breach the divide. Another 18:50 factor could be the so-called 18:51 atmospheric rivers. Okay, these fastm 18:55 moving air air currents can carry 18:57 immense amounts of water vapor. Western 19:00 disturbances or atmospheric rivers 19:02 connected with the subtropical jetream 19:04 can pick up monsoon moisture take it 19:06 across the Himalayas. 19:08 Okay. Uh global warming, steady rise in 19:11 greenhouse gases is heated land and 19:13 ocean. So very hot temperatures, 19:16 stronger updrafts, 19:18 right? Thinner snow and ice cover over 19:20 the Himalayas and Tibet. This opens 19:23 corridors for moisture to pass. It says 19:26 stronger winds at the Himalayan 19:28 foothills now lift moisture higher than 19:30 normal can trigger cloud burst and 19:33 valleys allow vapor to escape across the 19:35 ranges. 19:36 Um certain low passes, lower passes and 19:41 corridors within the Himalayans can act 19:44 as gateways. Um but they need to be uh 19:47 looked at and studied in more detail. 

19:49 Anyway, the monsoon crossing into Tibet 19:52 carries farreaching consequences. 19:55 It is first of all an evidence of a 19:57 shifting climate. Okay, so for centuries 20:00 the Himalayas have served as a climatic 20:03 wall. That shield appears weaker now. If 20:07 the barrier fails, South Asia's weather 20:09 cycle could undergo long-term changes. 20:13 Okay. So, the sudden in Tibet where 20:17 rainfall is scarce, sudden arrival of 20:20 monsoon moisture could gradually 20:22 transform ecosystems. 20:24 Right. A wetter Tibet could also 20:26 accelerate glacial melt, change the flow 20:28 of rivers that feed millions downstream. 20:33 For India, there's deeper concerns. The 20:35 monsoon delivers nearly 80% of the 20:37 country's rainfall just in the in in the 20:40 the seasonal monsoon. So that of course 20:43 is crucial for agriculture, water 20:46 supply. So if part of this moisture 20:48 bypasses India and flows into Tibet, 20:51 rainfall within India may decline. That 20:53 would threaten a lot of different 20:55 things. So anyway, there's no quick 20:57 conclusions on this. Uh but there are 21:00 some severe implications if it becomes a 21:03 regular phenomena. As of now, it's the 21:06 only time it's happened. It's 21:07 unprecedented. There a few more 21:09 articles. I'll just look at the 21:11 headlines. Monsoon crosses Himalayas 21:13 into Tibet. Bigger woes ahead. Um the 21:17 links are all in the description. 21:20 Um 21:22 I think I showed that one already. 21:25 Um, and there's lots of stuff on Reddit 21:28 for for what's happened. 21:30 Monsoon miracle or meteorological 21:33 disaster. Southwest winds defy Himalayan 21:35 barrier reach Tibet. Okay, so there's 21:37 lots of stuff on here. The Himalayan 21:40 shield weakening. 21:42 Now, I tried to look at some weather 21:44 data. There are National Geographic has 21:48 this website for Mount Everest weather 21:51 data and there's a whole bunch of 21:53 different stations which kind of leads 21:56 to the interesting question what weather 21:58 station is at the highest elevation and 22:02 then that's another question is you know 22:04 if jet streams are coming along it do we 22:07 actually have some weather stations on 22:09 top of mountains that are right in the 22:10 jetream before it splits and divides um 22:14 on these these um high elevation 22:17 um mountain ranges. Anyway, this data it 22:20 all goes back to 2023. So, it was they 22:23 got funding. They they did this had this 22:25 all these weather stations on Everest, 22:27 but there's not current data on them. 22:30 But, you know, it's it does beg the 22:32 question, what is I think in China, they 22:35 have the world's um highest elevation 22:38 weather station. Probably worth a 22:40 separate video on, you know, what sort 22:42 of things that it's it's finding. 22:45 Anyway, thank you for listening. Please 22:47 go to my website, paulbeckwith.net, 22:50 and donate to PayPal to support my 22:52 research and videos. And I'm on a 22:55 plethora of social media sites. Um, I 22:59 have Patreon. Um, I'm using I'm trying 23:02 to post on all kinds of different sites 23:05 and do reals and do Tik Tok videos and 23:08 stuff. So, you know, if you're on any of 23:11 these social media things, just search 23:13 for my name, Paul Beckwith. No spaces, 23:17 um, is is my most common handle on on on 23:21 all of these different social media 23:22 sites. So, thanks again for listening 23:25 and, uh, bye for now. All From Paul Beckwith
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