WEBVTT

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Okay, imagine this. Picture it playing out, maybe

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even right now. You've got this powerful hurricane,

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just this massive swirling thing, and it's heading

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straight for the coast, densely populated coast.

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Millions of people. Millions, and they're all

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hanging on, you know, bracing themselves, relying

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completely on those forecasts. Absolute precision

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needed for, well... life -saving decisions, evacuate,

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shelter, and then boom, just like that, no warning,

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one of our most critical eyes in the sky, this

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vital window into the storm's heart. It just

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goes dark. Just switched off. Switched off. Welcome,

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everyone, to Meteorology Matters. We're your

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guides today, and our mission, like always, is

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to take this, well, complex, sometimes really

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daunting information from all sorts of places

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and really distill it down, make it clear, give

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you actionable insights. Yeah. The goal is to

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help you become genuinely well -informed, not

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just the headlines, you know, but the actual

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science -shaping things. Exactly. And today,

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we're digging into a really sudden, very impactful...

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honestly, kind of mysterious decision came down

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just this week from the United States Department

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of Defense. Unexpected, is putting it mildly.

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They've decided to just terminate the processing

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and delivery of absolutely vital data, data streaming

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from a specific set of weather satellites. We're

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talking about the Special Sensor Microwave Imager

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Sounder, or everyone calls it SSMIS. Yes, SSMIS,

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yep. That's the one. And let's be crystal clear

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here. This isn't some, you know, minor technical

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tweak only specialists care about. No, no, this

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is profound. It's like a a seismic shift in how

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we observe these storms. Absolutely. It's a move

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that's going to severely impede significantly

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degrade hurricane forecasts. And not just for

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this year, the twenty twenty five season that's

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starting now, but. way beyond future seasons,

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too. We're talking direct impacts, tangible tens

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of millions of people living along those coastlines,

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their safety, their economic well -being. It

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relies on accurate predictions. And what's really

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baffling, truly perplexing is the lack of any

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immediate, clear reason. Why now? Why so abrupt?

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It seems to be tangled up with Department of

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Defense security concerns. But the really alarming

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part, even top officials at the National Hurricane

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Center were completely blindsided. No heads up,

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nothing. caught totally off guard. Yeah, it's

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just wild. It's unprecedented, really. And the

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ripples are already spreading through the whole

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weather and climate community. So over the next

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little while here on Meteorology Matters, our

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job is to dive deep, figure out exactly why this

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data from SSMIS, why it's so uniquely vital.

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Right. What are the concrete impacts going to

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be? It's loss on understanding, tracking, preparing

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for these massive weather events, hurricanes,

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climate patterns. And critically, What's the

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path forward? Because the global meteorological

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community is scrambling now, almost frantically,

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trying to adapt to this sudden hole in the data.

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So let's unpack it. Absolutely. Let's peel it

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back. Because to really get the gravity here,

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you first need to appreciate the, well, the absolutely

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essential role microwave satellite data plays

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in forecasting hurricanes. It's intricate stuff.

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And hurricanes themselves, they present this

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fundamental challenge for observation. It's plagued

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meteorologists for well forever decades. Yeah,

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these huge storms They mostly form and get stronger

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over these massive stretches of open water. Think

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about the scale hundreds thousands of miles from

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land. Where you just can't put ground measurements.

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It's not feasible. Right. No weather stations

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out in the middle of the Pacific or dotted across

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the deep Atlantic. We just don't have them. Exactly.

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That's the core dilemma. And yeah, we have the

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Hurricane Hunter planes, those amazing brave

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crews flying right into the eye. Incredible data

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from them. Invaluable, but they have real practical

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limits. These planes, they're only available

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for about one out of every three Atlantic hurricane

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forecasts. One in three. Yeah, think about that.

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Two -thirds of the time, we don't get that direct

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granular data from inside. And for Pacific storms,

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almost never. Maybe a handful of the really extreme

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cases. So most of the time, for these huge ocean

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storms without those planes, we're kind of flying

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blind, making critical calls with way less information.

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That's absolutely, yeah. It leaves this huge

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observational gap, a void that desperately needs

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filling for accurate forecasts. And that's where

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the satellites come in. But here's where it gets

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really interesting, where the power of this specific

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data, the stuff we're losing, really shines.

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There's a key difference, right, between the

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satellites most people are familiar with, the

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ones giving those beautiful swirling cloud pictures.

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Yeah, the geosynchronous ones you see on TV.

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Exactly. Those versus the more specialized polar

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orbiting satellites carrying these microwave

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sensors. OK, so what's the difference? Those

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regular visible or infrared satellites, they're

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great for tracking clouds, seeing the storm top.

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But they struggle. They can't really see through

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the dense clouds, especially at night when visible

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light is gone anyway. Ah. So they completely

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miss crucial details, stuff happening inside

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the storm structure, changes that can signal

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dangerous rapid intensification, you just can't

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see the inner workings with those conventional

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tools. Right, you only see the surface, the top

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layer. Precisely. And what's remarkable, what

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makes microwave data indispensable, is it gives

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us this unique capability. It's almost like an

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MRI scan of the atmosphere. An MRI, okay, I like

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that analogy. Yeah, like a doctor using an x

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-ray or MRI to see through PISHU to the organs

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inside. That's what microwave satellites do for

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us. They let forecasters literally peer through

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the obscuring clouds, through the heavy rain,

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right down near the surface. So they can see

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the storm's inner workings. Exactly. Where the

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heaviest rain is, the actual center location,

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and critically, its thermal and moisture structure.

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And they get these updates every few hours. It

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reveals what's happening inside, even when it's

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totally hidden by clouds. That's the x -ray vision

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you mentioned, seeing the internal heat, the

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moisture, stuff the normal pictures miss. It's

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the difference between seeing a car's paint job

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and understanding how the engine works. It's

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that level of insight. OK, so let's zero in on

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the instrument itself, the one going dark. SSMIS

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Special Sensor Microwave Imager Sounder. Break

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that down for us. OK, so it's a conical scanning

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passive microwave radiometer. Whoa, OK. Conical

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scanning? Yeah, imagine a sensor spinning like

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a lighthouse beam sweeps around, but it's looking

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down, sweeping this wide cone -shaped path below

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the satellite as it orbits. Got it. And passive.

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Passive means it's not sending out its own signal

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like radar does. It's just listening. Listening

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to the natural microwave energy that the Earth's

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surface and the atmosphere, including the storm,

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emit naturally. Different things emit different

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signals exactly water vapor rain ice particles

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They all have unique microwave signatures and

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this instrument picks them up across four main

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frequencies 19 .3 22 .2 37 .0 and 85 .5 gigahertz

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and it uses seven specific channels within those

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with different polarizations to like different

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channels on a radio tuned to different things

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kind of yeah Think of them as different wavelengths

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each tuned to see different aspects lower frequencies

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are good for heavy rain 22 .2 gigahertz is super

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sensitive to water vapor, and that 85 .5 gigahertz

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one. That gives incredible detail on ice scattering

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deep inside the storm core, really vital for

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structure. And this tech isn't brand new, right?

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You mentioned predecessors. All right, the first

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one, the SSMI, launched way back in June 1987,

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part of the Defense Meteorological Satellite

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Program, DMSP. So this capability, it's been

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foundational for decades. And that history, that

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long record, makes this loss even more significant.

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These DMST satellites with SSMIS, they orbit

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in a specific way. Yeah, near constant 53 degree

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angle, about 830 kilometers up. And this geometry

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lets them collect consistent data over a really

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wide path. about 1 ,400 kilometers across. So

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each pass covers a huge area. A huge area, giving

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comprehensive observations and the resolution,

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how much detail we get. It's 25 kilometers for

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things like total water vapor and sea surface

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wind and five brightness temperature channels.

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But for that crucial 85 .5 GHz channel, the one

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giving the sharpest internal view, it's even

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finer, 12 .5 km. Well, it aren't just numbers,

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are they? That defines the quality the detail

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forecasters have relied on. It's high definition

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storm diagnostics. Absolutely invaluable. So

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what do forecasters do with all this detailed

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penetrating data beyond just cool images? Oh,

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its contributions are indispensable. Huge for

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accuracy. For starters, it's critical for precisely

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fixing the storm center. pinpointing it exactly.

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That sounds simple, but you're saying it's not.

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It's notoriously difficult with just visible

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or infrared, especially if the center is hidden

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under a big cloud shield, which often happens.

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Like finding a needle in a haystack in the dark.

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Microwave lights up that needle. And getting

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that position right is crucial. Because it directly

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fights that. Butterfly effect we mentioned. Even

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small errors, maybe just tens of miles off initially

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for a weaker storm. They blow up over time. Dramatically.

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That tiny initial error, if you don't correct

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it with precise microwave data, it cascades into

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outsize forecast errors four or five days later.

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Big misses in the track forecast. But where the

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storm actually goes, that initial pinpoint matters

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that much. Immensely. It's like aiming that billiard

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ball off by a millimeter at the start. You're

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way off down the table. Without SSMIS, that initial

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millimeter error is much more likely. Wow. And

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it also powers some advanced tech AI stuff. Absolutely

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essential for that. One of the key tools for

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estimating storm intensity, especially when the

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Hurricane Hunters can't fly, is called DMINT,

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Deep Multispectral Intensity of Tropical Cyclones

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Estimator. DMINT sounds powerful. It is. It uses

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AI to analyze satellite data and predict storm

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strength. and it relies heavily, almost entirely,

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on the microwave data it ingests. Without SSMS,

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DMINT's ability to give accurate, timely intensity

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estimates severely hampered. Forecasters lose

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a key intensity tool. Leaving them less certain

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about the storm's true power. Exactly. And that

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directly increases the risk of what James Franklin,

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a retired NEC branch chief, famously called a

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sunrise surprise. A sunrise surprise? Sounds

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ominous. It is. It's that horrible moment seeing

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the first visible satellite pictures at dawn

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and realizing a storm got way stronger, way better

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organized overnight, maybe intensified dramatically.

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But you didn't see it happening. Because the

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key structural details were hidden from the infrared

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views overnight. Details only microwave data

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would have shown. It's finding out too late that

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the storm ramped up, giving people much less

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time to prepare for something far more dangerous.

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That's terrifying. And that scenario becomes

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more likely now. Much more likely. That microwave

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data was our safeguard against it. So the bottom

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line here, the immediate impact. DMSP, these

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three satellites with SSMIS, they provide roughly

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half of all the microwave scans forecasters get.

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Roughly half, yeah. Globally. And with the DoD

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pulling the plug on processing by June 30th,

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that vital data stream just goes dark. Poof.

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Gone. It's like a surgeon suddenly losing half

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their x -rays mid -operation, or a pilot losing

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half their instruments on approach. It's that

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level of challenge for hurricane forecasters

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now. This isn't just an inconvenience. The very

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data that helps spot those sudden terrifying

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bursts is rapid intensification. When a tropical

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storm explodes into a cat three or four overnight,

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that early warning capability is severely compromised.

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data availability sliced in half. It just greatly

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increases the odds of missing these events, underestimating

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storm strength, misplacing centers. It degrades

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forecast accuracy, period. It's a huge blow to

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hurricane preparedness, and it inherently puts

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more people at risk, right? Could cost people

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more money, dealing with worse forecasts? Absolutely.

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More risk, potentially higher costs for everyone

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involved, individuals, communities. Dealing with

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degraded forecasts has real consequences. And

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this isn't just about hurricanes, is it? The

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impact spread wider. Much wider. This data determination

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sends ripples everywhere, including critical

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climate monitoring, especially for sea ice in

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the polar regions. Sea ice? How does microwave

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data help there? Well, SSMIS data is fundamental.

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It's a core input for key data sets from the

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National Snow and Ice Data Center, NSIDC, run

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by the National Oceanic and Atmospheric Administration.

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Things like their near real -time sea ice concentration

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records, the overall sea ice index, crucial for

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tracking climate change, Arctic navigation. And

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those products rely on SSMIS. Heavily. And the

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immediate unsettling consequence. Those specific

00:12:39.149 --> 00:12:41.990
products just stop processing after June 30th,

00:12:42.070 --> 00:12:46.129
2025. Users, scientists, shippers, northern communities,

00:12:46.230 --> 00:12:48.539
they have to anticipate a data gap. Like losing

00:12:48.539 --> 00:12:51.039
a key chapter in the climate story makes it harder

00:12:51.039 --> 00:12:53.259
to see the whole picture. It's a major disruption

00:12:53.259 --> 00:12:55.980
for climate science. And navigating it, well,

00:12:56.279 --> 00:12:58.539
there's this urgent scramble to find and integrate

00:12:58.539 --> 00:13:02.860
alternatives for products built purely on SSMIS

00:13:02.860 --> 00:13:06.779
like sea ice concentration, OSI, 401D, and the

00:13:06.779 --> 00:13:10.220
interim record OSI 430A users just have to switch.

00:13:10.570 --> 00:13:12.970
find new products based on different data. Which

00:13:12.970 --> 00:13:15.889
isn't simple, right? Requires validation, introduces

00:13:15.889 --> 00:13:18.730
uncertainty. Exactly. It takes time, resources,

00:13:19.190 --> 00:13:21.049
not a clean swap. But some products are okay.

00:13:21.049 --> 00:13:23.070
You mentioned multi -sensor ones. Yeah, there's

00:13:23.070 --> 00:13:24.850
a bit of a silver lining there. Things like Sea

00:13:24.850 --> 00:13:28.750
Ice Edge, Type, and Drift OSI 402D, 403, 405D,

00:13:28.850 --> 00:13:31.210
they use multiple sensors already. And another

00:13:31.210 --> 00:13:33.649
instrument, AMSR2, is their primary source, so

00:13:33.649 --> 00:13:34.950
they're more resilient. They'll keep working

00:13:34.950 --> 00:13:37.529
without SSMIS. Okay, so they had a backup plan,

00:13:37.669 --> 00:13:39.919
essentially. That's fortunate. incredibly fortunate

00:13:39.919 --> 00:13:42.639
for those specific applications. And other products

00:13:42.639 --> 00:13:45.919
like sea ice emissivity and L2C ice concentration,

00:13:46.220 --> 00:13:49.240
they're either actively migrating to use AMSR2

00:13:49.240 --> 00:13:52.539
data now, or they already offer AMSR2 versions

00:13:52.539 --> 00:13:54.799
that users are being urged to switch to. So there's

00:13:54.799 --> 00:13:58.220
a push to adapt. A huge push. And what's really

00:13:58.220 --> 00:14:00.059
critical for the long -term climate picture is

00:14:00.059 --> 00:14:02.740
things like the Sea Ice Index, OSI 420. They're

00:14:02.740 --> 00:14:05.440
undergoing complex changes to integrate AMSR2.

00:14:05.860 --> 00:14:08.700
The absolute goal is a continuous time series,

00:14:09.200 --> 00:14:12.100
seamlessly building on the old SSMIS data. So

00:14:12.100 --> 00:14:14.120
we don't lose track of the long -term trends.

00:14:14.340 --> 00:14:17.100
Precisely. That continuity is vital. It's a massive

00:14:17.100 --> 00:14:19.840
effort, but essential to preserve decades of

00:14:19.840 --> 00:14:21.860
climate records. OK, so we've covered the practical

00:14:21.860 --> 00:14:24.539
impacts, hurricanes, climate. Let's really dive

00:14:24.539 --> 00:14:27.379
into the science now. data assimilation, why

00:14:27.379 --> 00:14:29.860
this specific data loss hurts so badly. Right.

00:14:30.000 --> 00:14:31.940
At the very foundation of all weather prediction

00:14:31.940 --> 00:14:34.600
models, these incredibly complex computer programs

00:14:34.600 --> 00:14:37.519
generating forecasts is this absolute reliance

00:14:37.519 --> 00:14:39.840
on accurate initial conditions. Starting point.

00:14:40.360 --> 00:14:42.879
Exactly. Precise data on the atmosphere state

00:14:42.879 --> 00:14:45.519
right now, especially moisture. Think of it like

00:14:45.519 --> 00:14:48.029
setting up dominoes. if those first few are off

00:14:48.029 --> 00:14:50.950
even slightly. The whole chain falls apart unpredictably.

00:14:51.049 --> 00:14:53.629
Perfectly put. And this is where our conventional

00:14:53.629 --> 00:14:56.009
observations weather balloons launched mostly

00:14:56.009 --> 00:14:59.190
over land twice a day. Surface stations, also

00:14:59.190 --> 00:15:01.620
mostly land -based, just fall short. especially

00:15:01.620 --> 00:15:03.740
for fast -changing storms over the ocean. They're

00:15:03.740 --> 00:15:06.940
too sparse, too infrequent for hurricanes. Entirely

00:15:06.940 --> 00:15:09.240
inadequate for sampling those dynamic, moisture

00:15:09.240 --> 00:15:11.919
-rich environments over the vast oceans. And

00:15:11.919 --> 00:15:14.740
even tiny uncertainties in that initial humidity

00:15:14.740 --> 00:15:16.720
field, which is super hard to measure globally,

00:15:17.139 --> 00:15:19.480
they can have a huge detrimental impact later

00:15:19.480 --> 00:15:22.340
on in the forecast. Errors grow exponentially.

00:15:22.480 --> 00:15:24.600
Which is where satellites become absolutely essential.

00:15:25.000 --> 00:15:27.570
Irreplaceable, even. Totally. Unlike fixed points,

00:15:27.929 --> 00:15:30.409
satellites sweep across the globe, filling those

00:15:30.409 --> 00:15:33.169
massive ocean gaps, providing spatially dense,

00:15:33.370 --> 00:15:35.850
repeatable data where we had almost nothing before.

00:15:36.129 --> 00:15:39.049
From scattered snapshots to a continuous global

00:15:39.049 --> 00:15:42.029
video feed. A great way to think about it. Now,

00:15:42.269 --> 00:15:45.210
getting all this indirect satellite data, not

00:15:45.210 --> 00:15:47.690
direct temperature or pressure, but microwave

00:15:47.690 --> 00:15:50.590
signals into the models, that requires sophisticated

00:15:50.590 --> 00:15:54.320
techniques. Data simulation. Specifically, things

00:15:54.320 --> 00:15:57.360
like 3DVAR, three -dimensional variational systems.

00:15:57.559 --> 00:16:00.120
3DVAR. Okay, break that down. Imagine the atmosphere

00:16:00.120 --> 00:16:03.379
is a giant complex puzzle. Our models predict

00:16:03.379 --> 00:16:06.259
how the pieces move. Traditional observations

00:16:06.259 --> 00:16:08.820
give us some pieces, but there are huge gaps,

00:16:08.860 --> 00:16:11.500
especially over oceans. Satellite data floods

00:16:11.500 --> 00:16:14.539
us with new clues, often indirect clues like

00:16:14.539 --> 00:16:17.039
microwave brightness temperatures. So 3DVAR is

00:16:17.039 --> 00:16:19.519
how we fit those clues into the puzzle. Exactly.

00:16:19.600 --> 00:16:22.029
It's like a super smart digital detective. It

00:16:22.029 --> 00:16:23.870
takes all observations, balloons, satellites,

00:16:24.090 --> 00:16:25.649
everything, and mathematically finds the single

00:16:25.649 --> 00:16:27.990
most consistent and most probable picture of

00:16:27.990 --> 00:16:30.629
the atmosphere right now. It optimizes the initial

00:16:30.629 --> 00:16:33.049
conditions, gets the puzzle started as accurately

00:16:33.049 --> 00:16:34.809
as possible. So the rest of the prediction works

00:16:34.809 --> 00:16:36.789
better. And there are different ways to feed

00:16:36.789 --> 00:16:39.370
SSMIS data into this. Two main ways, yeah. First

00:16:39.370 --> 00:16:42.789
is assimilating retrieved products, or RV. RV,

00:16:43.110 --> 00:16:45.669
what's that? It's computationally faster. You

00:16:45.669 --> 00:16:48.110
first convert the raw satellite signals into

00:16:48.110 --> 00:16:50.509
geophysical things like total water vapor or

00:16:50.509 --> 00:16:53.549
surface wind using statistical algorithms. Then

00:16:53.549 --> 00:16:56.549
you feed those into the model. Quicker, but maybe

00:16:56.549 --> 00:16:59.529
less accurate. Potentially. Because those statistical

00:16:59.529 --> 00:17:02.110
conversions, those retrievals, they might have

00:17:02.110 --> 00:17:05.670
errors or biases if the statistics aren't perfect

00:17:05.670 --> 00:17:08.630
or if other info used in the process is flawed.

00:17:09.029 --> 00:17:10.950
It's an estimation. OK, so what's the other way?

00:17:11.160 --> 00:17:13.720
The second method is directly assimilating the

00:17:13.720 --> 00:17:15.900
raw measurements, the brightness temperatures,

00:17:16.160 --> 00:17:20.319
or TB. TB raw data. Right. This is more computationally

00:17:20.319 --> 00:17:22.819
intensive but more physically robust. You feed

00:17:22.819 --> 00:17:24.880
the raw microwave signals directly into the model

00:17:24.880 --> 00:17:28.259
using a complex radiative transfer model. This

00:17:28.259 --> 00:17:30.400
simulates how microwaves actually travel through

00:17:30.400 --> 00:17:32.380
the atmosphere. So it's based more on physics

00:17:32.380 --> 00:17:35.700
than statistics. Exactly. Less dependent on potentially

00:17:35.700 --> 00:17:38.779
iffy stats. Better at reducing systematic biases.

00:17:39.289 --> 00:17:42.049
It takes more computer power, but often gives

00:17:42.049 --> 00:17:44.369
a pure, more accurate starting point because

00:17:44.369 --> 00:17:46.710
it uses the fundamental physics. More complex,

00:17:46.950 --> 00:17:49.349
but potentially better results. Generally, yes.

00:17:49.630 --> 00:17:51.549
And the math works out well enough to make it

00:17:51.549 --> 00:17:53.609
feasible. Okay, to really hammer home why this

00:17:53.609 --> 00:17:56.039
matters, you mentioned a case study. Hurricane

00:17:56.039 --> 00:17:59.259
Danny. Yeah, Hurricane Danny back in July 1997.

00:17:59.980 --> 00:18:01.960
Fascinating storm formed from a non -tropical

00:18:01.960 --> 00:18:04.660
system intensified in the Gulf. A perfect real

00:18:04.660 --> 00:18:07.380
-world test bed for seeing the impact of SSMI

00:18:07.380 --> 00:18:09.960
data assimilation. So what happened in the baseline?

00:18:10.420 --> 00:18:13.599
The forecasts without the microwave data. The

00:18:13.599 --> 00:18:16.940
control case. The results were stark. Pretty

00:18:16.940 --> 00:18:19.220
alarming, actually. The initial conditions from

00:18:19.220 --> 00:18:22.460
standard systems like NOAAs, GDAs, they severely

00:18:22.460 --> 00:18:24.690
lacked moisture over the Gulf. And the storm's

00:18:24.690 --> 00:18:27.369
initial spin, the low level circulation, was

00:18:27.369 --> 00:18:29.730
way too weak. Which led to? Big underestimates

00:18:29.730 --> 00:18:32.029
of intensity. For example, the model's central

00:18:32.029 --> 00:18:35.630
pressure for Danny was 19 .5 hectopascals higher

00:18:35.630 --> 00:18:38.849
than observed after 48 hours. A huge miss. Plus

00:18:38.849 --> 00:18:40.809
the model needed at least eight hours of spin

00:18:40.809 --> 00:18:42.950
up time before it even started raining realistically.

00:18:43.190 --> 00:18:45.109
It was starting cold. Eight hours just to get

00:18:45.109 --> 00:18:47.829
going properly. That's a long delay. A very long

00:18:47.829 --> 00:18:50.910
delay. But here's where the SSMI data made a

00:18:50.910 --> 00:18:53.529
transformative difference. When they assimilated,

00:18:53.680 --> 00:18:56.880
Either the retrieved products, RV, or the raw

00:18:56.880 --> 00:19:00.019
brightness temps, TB. What changed? Instantly,

00:19:00.259 --> 00:19:03.019
almost. The atmospheric moisture across most

00:19:03.019 --> 00:19:05.619
of the Gulf dramatically increased in the model

00:19:05.619 --> 00:19:08.119
starting point. The low level circulation got

00:19:08.119 --> 00:19:11.140
much stronger, much more realistic. The inflow

00:19:11.140 --> 00:19:13.420
feeding the storm improved. It gave the model

00:19:13.420 --> 00:19:15.380
the right ingredients from the start. Exactly.

00:19:15.759 --> 00:19:18.240
And crucially, that spin up time. It plummeted.

00:19:18.500 --> 00:19:21.240
With SSMI data in, the model started producing

00:19:21.240 --> 00:19:23.299
light rain within just one or two hours. Wow,

00:19:23.319 --> 00:19:26.259
from eight hours down to one or two. That's huge

00:19:26.259 --> 00:19:29.240
for getting timely rain forecasts out. Massive.

00:19:29.400 --> 00:19:32.140
And the intensity forecasts. They got incredibly

00:19:32.140 --> 00:19:34.240
better, much more accurate capturing the storm's

00:19:34.240 --> 00:19:36.970
deepening pressure. The raw data. TB approach

00:19:36.970 --> 00:19:39.269
got the final pressure within one hectopascal

00:19:39.269 --> 00:19:42.809
of reality after 48 hours. The retrieved data,

00:19:42.990 --> 00:19:46.170
RV, was 8 HPA deeper than observed, still vastly

00:19:46.170 --> 00:19:49.309
better than the control's 19 .5 HPA error. So

00:19:49.309 --> 00:19:51.569
both methods were dramatically better than no

00:19:51.569 --> 00:19:54.029
data at all. A revolution, really. Absolutely.

00:19:54.410 --> 00:19:56.190
And the visual structure in the simulations.

00:19:56.809 --> 00:20:00.450
Night and day. With SSMI, the models produced

00:20:00.700 --> 00:20:03.660
clear hurricane eyes, distinct eye walls, spiral

00:20:03.660 --> 00:20:06.180
bands, which is totally missing in the control

00:20:06.180 --> 00:20:08.700
run. Like seeing an ultrasound versus just guessing?

00:20:09.059 --> 00:20:11.740
A perfect analogy. Forecasters could suddenly

00:20:11.740 --> 00:20:14.180
see the storm's internal evolution much more

00:20:14.180 --> 00:20:16.400
clearly. Now what about the computational cost?

00:20:16.839 --> 00:20:19.519
All that raw data processing sounds expensive.

00:20:19.640 --> 00:20:21.759
You'd think so, but the study actually showed

00:20:21.759 --> 00:20:24.180
that while the raw TB method took about twice

00:20:24.180 --> 00:20:27.500
the CPU time as the RV method, the total assimilation

00:20:27.500 --> 00:20:30.480
time was still only about 3 .5 minutes. compared

00:20:30.480 --> 00:20:33.039
to the 157 hours it took to run the 48 -hour

00:20:33.039 --> 00:20:35.980
forecast itself. Negligible. So it's totally

00:20:35.980 --> 00:20:38.400
affordable, computationally speaking. A tiny

00:20:38.400 --> 00:20:40.480
investment for massive forecast improvement.

00:20:40.799 --> 00:20:42.700
Completely affordable and highly beneficial.

00:20:42.900 --> 00:20:45.259
It pays for itself many times over in improved

00:20:45.259 --> 00:20:47.799
warning. But it wasn't a magic bullet for everything,

00:20:47.819 --> 00:20:50.619
right? The study noted some limitations. True.

00:20:51.200 --> 00:20:53.619
While intensity and structure improved dramatically,

00:20:54.059 --> 00:20:56.420
the impact on the storm track forecast was surprisingly

00:20:56.420 --> 00:21:00.190
small. All the simulations, even with SSMI data,

00:21:00.549 --> 00:21:03.549
had this consistent leftward track bias. They

00:21:03.549 --> 00:21:05.369
predicted Danny to go slightly left of where

00:21:05.369 --> 00:21:07.230
it actually went. And that matched the official

00:21:07.230 --> 00:21:09.690
forecasts at the time. Yeah, suggesting a deeper

00:21:09.690 --> 00:21:13.049
issue. Probably inaccuracies in the initial steering

00:21:13.049 --> 00:21:15.369
winds higher up in the atmosphere. Stuff that

00:21:15.369 --> 00:21:17.650
SSMI doesn't directly measure well. Exactly.

00:21:17.869 --> 00:21:19.630
It points to the need for other instruments,

00:21:19.869 --> 00:21:21.650
like LiR, that can measure those steering winds

00:21:21.650 --> 00:21:24.359
directly. You need complementary data. And even

00:21:24.359 --> 00:21:26.819
with SSMI, the model still struggled to capture

00:21:26.819 --> 00:21:29.359
every cloud band perfectly, or subtle things

00:21:29.359 --> 00:21:31.980
like cirrus clouds, no single instrument sees

00:21:31.980 --> 00:21:34.140
everything. It's always about combining perspectives.

00:21:34.319 --> 00:21:37.599
Always. But the key takeaway from Danny is undeniable.

00:21:38.359 --> 00:21:41.539
Assimilating that SSMI data had a strong, unequivocally

00:21:41.539 --> 00:21:44.140
positive impact, especially on intensity and

00:21:44.140 --> 00:21:46.839
structure. While the two methods, RV versus TB,

00:21:46.880 --> 00:21:49.500
had differences, both were vastly superior to

00:21:49.500 --> 00:21:52.079
having no data. It proved this microwave data

00:21:52.079 --> 00:21:55.130
is foundational. Foundational, not just incremental.

00:21:55.890 --> 00:21:58.069
Okay, so laying all that out, knowing its value,

00:21:59.490 --> 00:22:02.710
what's the path forward now? We have this immediate

00:22:02.710 --> 00:22:05.869
lasting data gap. Yeah, and it casts a long shadow

00:22:05.869 --> 00:22:08.470
over this hurricane season and beyond. Losing

00:22:08.470 --> 00:22:11.009
SSMIS means losing half our microwave instruments.

00:22:11.690 --> 00:22:14.049
It dangerously increases the odds of missing

00:22:14.049 --> 00:22:16.890
rapid intensification, underestimating intensity,

00:22:17.329 --> 00:22:19.589
misplacing storms. Putting more people at risk,

00:22:19.730 --> 00:22:22.150
increasing potential costs. Plain and simple.

00:22:22.369 --> 00:22:24.450
But the community isn't just sitting back. They're

00:22:24.450 --> 00:22:27.089
urgently searching for replacements. The main

00:22:27.089 --> 00:22:29.890
contender right now is AMSR2 Advanced Microwave

00:22:29.890 --> 00:22:33.150
Scanning Radiometer 2. AMSR2, does it offer improvements?

00:22:33.309 --> 00:22:36.250
It does. Better resolution than SSMIS, so potentially

00:22:36.250 --> 00:22:38.490
more detail. That's good. Out there is a catch.

00:22:38.710 --> 00:22:41.309
There is. AMSR2 data is still considered prototype.

00:22:41.490 --> 00:22:43.890
It's undergoing testing. And crucially, it hasn't

00:22:43.890 --> 00:22:46.710
been fully intercalibrated with the older SSMIS

00:22:46.710 --> 00:22:48.789
data yet. Meaning the measurements might not

00:22:48.789 --> 00:22:52.039
line up perfectly. Exactly. Users might see differences,

00:22:52.079 --> 00:22:55.680
say in CI610, comparing AMSR2 to the historical

00:22:55.680 --> 00:22:59.039
SSMIS record. partly because its higher resolution

00:22:59.039 --> 00:23:01.839
sees edges better. So while it's promising, it's

00:23:01.839 --> 00:23:04.099
not a seamless swap yet. It's a work in progress.

00:23:04.200 --> 00:23:06.079
And progress takes time we don't necessarily

00:23:06.079 --> 00:23:08.619
have right now. What about other options? There's

00:23:08.619 --> 00:23:11.740
the weather system follow on microwave, WSFM,

00:23:11.880 --> 00:23:16.259
designed specifically as the successor to DMSPS

00:23:16.259 --> 00:23:19.480
SMIS. It launched successfully in April 2024.

00:23:19.819 --> 00:23:22.039
Fantastic. So that should fill the gap. It should.

00:23:22.400 --> 00:23:24.990
But here's the frustrating part. The data from

00:23:24.990 --> 00:23:28.250
WSF -M is not currently available to forecasters.

00:23:28.430 --> 00:23:30.150
Wait, it's up there, but we can't use the data.

00:23:30.190 --> 00:23:32.930
Correct. It's uncertain if or when access will

00:23:32.930 --> 00:23:35.170
be permitted. Bureaucratic hurdles, security

00:23:35.170 --> 00:23:38.049
protocols, complex reasons. But the bottom line

00:23:38.049 --> 00:23:41.210
for forecasters, a capable satellite designed

00:23:41.210 --> 00:23:43.650
for this exact purpose is flying blindfolded

00:23:43.650 --> 00:23:45.990
right now. The data isn't flowing. That's incredibly

00:23:45.990 --> 00:23:48.269
frustrating. So connecting this all back, the

00:23:48.269 --> 00:23:51.170
broader stakes for society are huge. Undeniable.

00:23:51.769 --> 00:23:54.640
This data loss... puts more people at risk. It

00:23:54.640 --> 00:23:57.099
could lead to higher costs, unnecessary evacuations,

00:23:57.259 --> 00:24:00.079
or worse, failing to evacuate when needed. The

00:24:00.079 --> 00:24:02.740
ripples hit emergency services, insurance, supply

00:24:02.740 --> 00:24:05.420
chains, daily lives. It really underscores how

00:24:05.420 --> 00:24:08.019
much we rely on this infrastructure. On a slightly

00:24:08.019 --> 00:24:09.799
brighter note, anything happening right now?

00:24:10.420 --> 00:24:13.859
A tiny fleeting positive. Current models show

00:24:13.859 --> 00:24:15.640
the Atlantic staying quiet through the end of

00:24:15.640 --> 00:24:18.380
June. No tropical development expected for the

00:24:18.380 --> 00:24:21.660
next week or so. Okay, so a small window of reprieve

00:24:21.660 --> 00:24:24.140
as this data stream shuts down. A small window,

00:24:24.400 --> 00:24:26.859
but just a brief calm before what could be a

00:24:26.859 --> 00:24:29.079
very challenging, very unpredictable season,

00:24:29.579 --> 00:24:32.380
now with fewer tools in the toolbox. So to wrap

00:24:32.380 --> 00:24:34.579
up our Meteorology Matters discussion today,

00:24:34.940 --> 00:24:36.920
we've looked at the sudden, really impactful

00:24:36.920 --> 00:24:40.319
loss of critical SSMIS data. An indispensable

00:24:40.319 --> 00:24:43.220
eye in the sky, now dark. We've detailed the

00:24:43.220 --> 00:24:45.099
profound implications for hurricane intensity

00:24:45.099 --> 00:24:47.940
forecasts for vital sea ice monitoring that tracks

00:24:47.940 --> 00:24:50.200
climate change. And we've looked at the urgent

00:24:50.200 --> 00:24:52.779
ongoing scramble to find, test, and integrate

00:24:52.779 --> 00:24:55.059
alternatives to fill this sudden gaping hole

00:24:55.059 --> 00:24:57.529
in our observations. And this whole situation,

00:24:57.769 --> 00:24:59.769
it really makes you think, doesn't it? It raises

00:24:59.769 --> 00:25:02.349
a question for you, our listener. How often do

00:25:02.349 --> 00:25:05.470
we really stop to consider the complex, often

00:25:05.470 --> 00:25:08.609
invisible scientific web that supports our safety,

00:25:08.849 --> 00:25:12.369
our economy, just our daily lives? Yeah. What

00:25:12.369 --> 00:25:15.529
other crucial unseen data sources are we just

00:25:15.529 --> 00:25:18.910
assuming will always be there? Data that, like

00:25:18.910 --> 00:25:22.289
SSMIS, could just vanish overnight. And what's

00:25:22.289 --> 00:25:25.940
the real cost? of unquantifiable when these critical

00:25:25.940 --> 00:25:28.759
systems are disrupted. Something to ponder. Definitely

00:25:28.759 --> 00:25:30.420
something to ponder. Now, if you want to stay

00:25:30.420 --> 00:25:33.339
right on the cutting edge of meteorology, hurricane

00:25:33.339 --> 00:25:35.619
tracking, and keep getting clarity on vital topics

00:25:35.619 --> 00:25:38.200
like this, you absolutely need to follow meteorologist

00:25:38.200 --> 00:25:40.839
Rob Jones. You can find him on Instagram to search.

00:25:41.859 --> 00:25:45.599
He's also on TikTok as TVMeteorologist. And definitely

00:25:45.599 --> 00:25:47.720
check out his YouTube channel, search Rob Jones

00:25:47.720 --> 00:25:49.839
Hurricane. That's where you'll also find the

00:25:49.839 --> 00:25:51.960
Meteorology Matters podcast playlist with all

00:25:51.960 --> 00:25:54.460
our discussions. Excellent resources. Well, thank

00:25:54.460 --> 00:25:56.440
you for joining us on this Meteorology Matters

00:25:56.440 --> 00:25:58.480
deep dive. We look forward to exploring more

00:25:58.480 --> 00:25:59.819
essential knowledge with you next time.
