The Atlantic
Outside satellite experts say investigators could be looking in the wrong ocean.
This graph is the most important piece of evidence in the Inmarsat analysis.
What it appears to show is the frequency shifts or “offsets”—the
difference between the normal “pitch” of the plane’s voice (its radio
frequency) and the one you actually hear.
Why Inmarsat’s Analysis Is Probably Wrong
Outside satellite experts say investigators could be looking in the wrong ocean.
Investigators searching for the missing Malaysian Airlines
flight were ebullient when they detected what sounded like signals from
the plane’s black boxes. This was a month ago, and it seemed just a
matter of time before the plane was finally discovered.
But now the search of 154 square miles of ocean floor around
the signals has concluded with no trace of wreckage found. Pessimism is
growing as to whether those signals actually had anything to do with
Flight 370. If they didn’t, the search area would return to a size of tens of thousands of square miles.
Even before the black-box search turned up empty, observers
had begun to raise doubts about whether searchers were looking in the
right place. Authorities have treated the conclusion that the plane
crashed in the ocean west of Australia as definitive, owing to a
much-vaunted mathematical analysis of satellite signals sent by the
plane. But scientists and engineers outside of the investigation have
been working to verify that analysis, and many say that it just doesn’t
hold up.
A Global Game of Marco Polo
Malaysia Airlines flights are equipped with in-flight
communications services provided by the British company Inmarsat. From
early on, the lynchpin of the investigation has been signals sent by
Flight 370 to one of Inmarsat’s satellites. It’s difficult to overstate
the importance of this lonely little batch of “pings.”
They’re the sole
evidence of what happened to the plane after it slipped out of radar
contact. Without them, investigators knew only that the plane had enough
fuel to travel anywhere within 3,300 miles of the last radar contact—a seventh of the entire globe.
Inmarsat concluded that the flight ended in the southern
Indian Ocean, and its analysis has become the canonical text of the
Flight 370 search.
It’s the bit of data from which all other judgments
flow—from the conclusive announcement by Malaysia’s prime minister that the plane has been lost with no survivors, to the black-box search area, to the high confidence in the acoustic signals, to the dismissal by Australian authorities of a survey company’s new claim to have detected plane wreckage.
Although Inmarsat officials have described the mathematical analysis as “groundbreaking,”
it’s actually based on some relatively straightforward geometry. Here’s
how it works: Every so often (usually about once an hour), Inmarsat’s
satellite sends a message to the plane’s communication system, asking
for a simple response to show that it’s still switched on.
This response
doesn’t specify the plane’s location or the direction it’s heading, but
it does have some useful information that narrows down the
possibilities.
You can think of the ping math like a game of Marco Polo
played over 22,000 miles of outer space. You can’t see the plane. But
you shout Marco, and the plane shouts back Polo. Based
on how long the plane takes to respond, you know how far away it is.
And from the pitch of its voice, you can tell whether it’s moving toward
you or away from you—like the sound of a car on the highway—and about
how fast.
This information is far from perfect. You know how far the
plane was for each ping, but the ping could be coming from any
direction. And you how fast the plane is moving toward or away from you.
It could also be moving right or left, up or down, and the speeds would
sound the same.
The task of the Inmarsat engineers has been to take
these pieces and put them together, working backwards to reconstruct
possible flight paths that would fit the data.
What’s the Frequency?
There are two relevant pieces of information for each ping:
the time it took to travel from plane to satellite, and the radio
frequency at which it was received.
It’s important to keep in mind that
the transit times of the pings correspond todistances between satellite
and plane, while frequencies correspond to relative speeds between
satellite and plane. And this part’s critical: Relative speed isn’t the
plane’s actual airspeed, just how fast it’s moving toward or away from
the satellite.
Authorities haven’t released much information about the distances—just the now-famous “two arcs” graphic,
derived in part from the distance of the very last ping. But they’ve
released much more information about the ping frequencies. In fact, they
released a graph that shows all of them:
The graph also shows the shifts that would be expected for two
hypothetical flight paths, one northbound and one southbound, with the
measured values closely matching the southbound path. This is why
officials have been so steadfastly confident that the plane went south.
It seems to be an open-and-shut verdict of mathematics.
So it should be straightforward to make sure that the math
is right. That’s just what a group of analysts outside the investigation
has been attempting to verify. The major players have been Michael Exner, founder of the American Mobile Satellite Corporation; Duncan Steel, a physicist and visiting scientist at NASA’s Ames Research Center; and satellite technology consultant Tim Farrar.
They’ve used flight and navigation software like STK,
which allows you to chart and make precise calculations about flight
scenarios like this one. On their blogs and in an ongoing email chain,
they’ve been trying to piece together the clues about Flight 370 and
make sense of Inmarsat’s analysis. What follows is an attempt to explain
and assess their conclusions.
What We Know
Although the satellite data provides the most important clues about the plane’s overall flight path, they’re not the only clues available. Authorities have some basic but crucial additional information about the flight that can help to make sense of the satellite math:
1. The satellite’s precise coordinates.
The satellite in contact with Flight 370 was Inmarsat’s IOR satellite,
parked in geostationary orbit above the Indian Ocean. The satellite is
meant to be stationary, but its orbit has decayed somewhat, so that it
actually rotates slightly around its previously fixed position. Its path
is publicly available from the Center for Space Standards & Innovation.
2. The plane’s takeoff time and coordinates
16:41 UTC from the Kuala Lumpur airport.
3. The plane’s general motion toward or away from the satellite
From radar tracking,
we know the plane traveled northeast, away from the satellite, over the
first 40 minutes after takeoff, then westward, toward the satellite,
until 94 minutes into the flight, when it was last detected on radar.
Inmarsat spokesmen have stated that the ping distances got progressively longer over the last five hours of flight, meaning that the plane was moving away from the satellite during that time.
4. Two flight paths investigators think are consistent with the ping data
In addition to the frequency shift graph, the Inmarsat
report includes a map with two “Example Southern Tracks,” one assuming a
flight speed of 400 knots, the other a speed of 450 knots. Check it
out:
These bits of knowledge allow us to put some basic
constraints on what a graph of the ping frequency shifts should look
like. We’ll use more precise numbers later; for now, it’s helpful just
to have some qualitative sense of what to expect:
5. Frequency shifts that should all be negative.
When the plane is moving away from the satellite, the radio
signal gets stretched out, so the frequency decreases. This means that
the frequency shifts should be negative over most of the flight.
Although there was an approximately one-hour period starting 40 minutes
after takeoff when radar showed the plane moving westward, toward the
satellite, the graph shows that no pings were sent during that time—so
actually, all of the shifts on the graph should be negative.
6. Frequency shifts before takeoff that should be near zero.
Plotting the satellite’s path in STK, you can see that it
moves through an ellipse centered around the equator. Space scientist
Steel has created this graphic of the satellite’s motion, including
marks for its position when the plane took off and when it last pinged
the satellite:
The satellite’s motion is almost entirely north-south, and
the plane’s takeoff location in Kuala Lumpur is almost due east of the
satellite. This means that the satellite was only barely moving relative
to Kuala Lumpur, so the frequency shift for a plane nearly stationary
on the ground at the airport would be nearly zero.
7. Frequency shift graph should match map of southbound flight paths.
The way the Marc-Polo math works is that, if you assume the
plane traveled at some constant speed, you can produce at most one path
north and one path south that fit the ping data. As the example flight
paths on Inmarsat’s map show, the faster you assume the plane was moving
overall, the more sharply the path must arc away from the satellite.
This constraint also works the other way: Since flight
paths for a given airspeed are unique, you can work backwards from these
example paths, plotting them in STK to get approximate values for the
ping distances and relative speeds Inmarsat used to produce them.
The
relative speeds can then be converted into frequency shifts, which
should roughly match the values on the frequency graph. (This is all
assuming that Inmarsat didn’t plot the two example paths at random but
based on the ping data.) We’ll put more precise numbers on this below.
The Troubled Graph
But the graph defies these expectations. Taken at face
value, the graph shows the plane moving at a significant speed before it
even took off, then movingtoward the satellite every time it was
pinged. This interpretation is completely at odds with the official
conclusion, and flatly contradicted by other evidence.
The first problem seems rather straightforward to resolve:
the reason the frequency shifts aren’t negative is probably that
Inmarsat just graphed them as positive. Plotting absolute values is a
common practice among engineers, like stating the distance to the ocean
floor as a positive depth value rather than a negative elevation value.
But the problem of the large frequency shift before takeoff
is more vexing. Exactly how fast does the graph show the plane and
satellite moving away from each other prior to takeoff?
The first ping on the graph was sent at 16:30 UTC, eleven
minutes prior to takeoff. The graphed frequency shift for this ping is
about -85 Hz. Public recordsshow
that the signal from the plane to the satellite uses a frequency of
1626 to 1660 MHz.
STK calculations show the satellite’s relative motion
was just 2 miles per hour toward the airport at this time. Factoring in
the satellite’s angle above the horizon, the plane would need to have
been moving at least 50 miles per hour on the ground to produce this
frequency shift—implausibly high eleven minutes prior to takeoff, when flight transcripts show the plane had just pushed back from the gate and not yet begun to taxi.
On the other side of the frequency graph, the plane’s last
ping, at 00:11 UTC, shows a measured frequency shift of about -252 Hz,
working out to a plane-to-satellite speed of just 103 miles per hour.
But the sample southbound paths published by Inmarsat show the plane
receding from the satellite at about 272 miles per hour at this time.
In other words, the frequency shifts are much higher than
they should be at the beginning of the graph, and much lower than they
should be at the end. Looking at the graph, it’s almost as if there’s
something contributing to these frequency shift values other than just
the motion between the satellite and the plane.
Cracking the ‘Doppler Code’
Exner, an engineer who’s developed satellite and
meteorology technologies since the early 1970s, noted that the measured
frequency shifts might come not just from each ping’s transmission from
plane to satellite, but also from the ping’s subsequent transmission
from the satellite to a ground station that connects the satellites into
the Inmarsat network. In other words, Exner may have found the hidden
source that seems to be throwing off the frequency graph.
Inmarsat’s analysis is highly ambiguous about whether the
satellite-to-ground transmission contributed to the measured frequency
shift. But if it did, a ground station located significantly south of
the satellite would have resulted in frequency shifts that could account
for the measured shifts being too large at the beginning of the graph
and too small at the end.
And sure enough, Inmarsat’s analysis states
that the ground station receiving the transmission was located in
Australia.
It’s possible to check the theory more precisely.
Public records of Inmarsat ground stations show just one in Australia: in Perth. Using STK, you can precisely chart the satellite’s speed relative to this station, and, using thesatellite-to-ground signal frequency (about
3.6 GHz), you can then factor the satellite-to-ground shifts out of the
frequency graph. Finally, you can at last calculate the true
satellite-to-plane speed values.
The results seem to be nearly perfect. For the first ping,
you wind up with a satellite-to-plane speed of about 1 mile per
hour—just what you’d expect for a plane stationary or slowly taxiing
eleven minutes before takeoff. This finding seems to provide a basic
sanity check for interpreting the graph, and led Exner to declare on Twitter,
“Doppler code cracked.”
He produced a new graph of the frequency
shifts, shown below. The gently sloping blue line shows the shifts
between the satellite and the ground station in Perth, while the dotted
red line shows the newly calculated satellite-to-plane shifts:
If this interpretation—based on the work of Exner, Steel,
Farrar, and myself—is correct, it would allow independent experts to
fully review Inmarsat’s analysis, verify its work and check to see if
Inmarsat might have missed any important clues that could further narrow
down the plane’s whereabouts.
The problem is, although this interpretation matches two
basic expectations for the frequency graph, it still doesn’t match
Inmarsat’s example flight paths. The new frequency values, calculated by
Exner, show the flight’s speed relative to the satellite as only about
144 miles per hour by the last ping, but Inmarsat’s example flight paths
show a relative speed of about 272 miles per hour.
It’s possible these outside experts have still erred or
missed some crucial detail in their attempts to understand the Inmarsat
analysis. But that just means that Inmarsat’s analysis, as it has been
presented, remains deeply confusing, or perhaps deeply confused.
And
there are other reasons to believe that Inmarsat’s analysis is not just
unclear but mistaken. (Inmarsat stands by its analysis. More on that in a
minute.)
Recall that the Marco-Polo math alone doesn’t allow you to
tell which direction pings are coming from. So how could Inmarsat claim
to distinguish between a northern and southern path at all? The reason
is that the satellite itself wasn’t stationary.
Because the satellite
was moving north-south, it would have been moving faster toward one path
than another—specifically, faster toward a southbound track than a
northbound one over the last several hours of the flight. This means
that the frequency shifts would also differ between a northbound and
southbound path, as the graph shows with its two predicted paths.
But this is actually where the graph makes the least sense.
The graph only shows different predicted values for the north and south
tracks beginning at 19:40 UTC (presumably Inmarsat’s model used actual
radar before this). By this time, the satellite was traveling south, and
its southward speed would increase for the rest of the flight.
The
frequency shift plots for northern and southern paths, then, should get
steadily further apart for the rest of the flight. Instead, the graph
shows them growing closer. Eventually, they even pass each other: by the
end of the flight, the graph shows the satellite traveling
faster toward a northbound flight path than a southbound one, even
though the satellite itself was flyingsouth.
One ping alone is damning. At 19:40 UTC, the satellite was
almost motionless, having just reached its northernmost point. The graph
shows a difference of about 80 Hz between predicted northbound and
southbound paths at this time, which would require the satellite to be
moving 33 miles per hour faster toward the southbound path than the
northbound one. But the satellite’s overall speed was just 0.07 miles
per hour at that time.
Inmarsat claims that it found a difference between a
southbound and northbound path based on the satellite’s motion. But a
graph of the frequency shifts along those paths should look very
different from the one Inmarsat has produced.
Losing Faith
Either Inmarsat’s analysis doesn’t totally make sense, or it’s flat-out wrong.
For the last two months, I’ve been trying to get
authorities to answer these questions. Malaysia Airlines has not
returned multiple requests for comment, nor have officials at the
Malaysian Ministry of Transportation.
Australia’s Joint Agency
Coordination Centre and the UK’s Air Accidents Investigation Branch,
which have been heavily involved in the investigation, both declined to
comment.
An Inmarsat official told me that to “a high degree of
certainty, the proponents of other paths are wrong. The model has been
carefully mapped out using all the available data.”
The official cited Inmarsat’s participation in the
investigation as preventing it from giving further detail, and did not
reply to requests for comments on even basic technical questions about
the analysis.
Inmarsat has repeatedly claimed that it checked its model
against other aircrafts that were flying at the time, and peer-reviewed
the model with other industry experts. But Inmarsat won’t say who
reviewed it, how closely, or what level of detail they were given.
Until officials provide more information, the claim that
Flight 370 went south rests not on the weight of mathematics but on
faith in authority.
Inmarsat officials and search authorities seem to
want it both ways: They release charts, graphics, and statements that
give the appearance of being backed by math and science, while refusing
to fully explain their methodologies. And over the course of this
investigation, those authorities have repeatedly issued confident
pronouncements that they’ve later quietly walked back.
The biggest risk to the investigation now is that
authorities continue to assume they’ve finally found the area where the
plane went down, while failing to explore other possibilities simply
because they don’t fit with a mathematical analysis that may not even
hold up.
After all, searchers have yet to find any hard evidence—not
so much as a shred of debris—to confirm that they’re looking in the
right ocean.
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