NOAA — Straight Talk on Sea Level Rise

Guest Essay by Kip Hansen

 

North_Atlantic_RSLR_TrendsThe National Oceanic and Atmospheric Administration has some rather useful features on its web site.

One of these is the Tides and Currents which is part of its Center for Operational Oceanographic Products and Services.  Having spent most of the current century living at sea,  with my wife and occasionally a son or our daughter and granddaughter, on our venerable sailing catamaran, the Golden Dawn,   cruising the eastern coast of the United States, the Bahamas, the Turks and Caicos, Hispaniola, and the Spanish, U.S., and British Virgin Islands, I have made extensive use of its features.

For our purposes, the most used features were the predictions of the size and timing of tides in various places which often determined our sailing schedule to allow us to leave or arrive at various states of tides, often necessary to clear the bar to a harbor entrance, pass over a coral reef, or move through a pass between islands with, instead of against, the tide.   When sailing up the Hudson River in New York to our oft-times home, we must be aware of  the flow of the river, the current, which is tidal, going north on the incoming tide and south on the outgoing tide.  The current can be so strong against us that we often just anchor and fire up the barbie and put out a fishing line and wait for more favorable currents.

TurkeyPoint_Tide-StationThis is the data (excerpted) for Turkey Point on the Hudson.  The Kingston-Rhinecliff Bridge is in the background (looking south).  The tide chart shows four feet of tide, 100 miles north of New York City.

I am so familiar with the NOAA Tides and Currents site that I have tended to overlooked many features over the years.  In writing about SEA LEVEL: Rise and Fall, I have often used the Sea Level Trends portion of the site, like this one for Montauk, NY.

Montauk_NY_RSLT

This graph is marked “Relative Sea level Trend”.  So, let’s start with a [hopefully] cute little “Pic-torial” (a picture-based tutorial) on the “what and how” of Relative Sea Level – it should only take 60 seconds or so to view and read:

What Exactly is Relative Sea Level (rise or fall)?

Tide stations measure Local (Relative) Sea Level, which refers to the height of the water as measured along the coast relative to a specific point on land

There are three possible combinations of relative sea level rise under current geological conditions:

ASLR_400

This image shows Absolute Sea Level rising and its effect on Relative Sea Level at this Tide Gauge. As time goes by, the surface of the sea rises while the land remains motionless.  This results in Relative Sea Level rise.

 

 

 

 

 

VLM_400

This image shows Relative Sea Level rising but it is the land moving down, towards the center of the Earth, which is causing the sea surface to rise in relation to the land. Downward Vertical Land Movement causes Relative Sea Level rise.   Downward VLM is most often caused by movement of the Earth’s crust, compaction of the soil (which is often created by filling along the water’s edge for docks and piers) and in some cases, water and petroleum extraction.

 

VLM_ASLR_400

This third image shows Relative Sea Level rising in the most usual case:  the sea surface is a rising a bit and the land is moving down a bit.  This is the case for most of the tide gauges on the US Eastern Seaboard, south of Boston.  Combined absolute sea level rise and downward VLM make Relative Sea Level rise.

NOAA pegs global absolute sea level rise at about 1.7 mm/yr.  VLM, along most of the US Eastern seaboard is of similar magnitude, in that it is measured in single-digit mm/yr, in most cases less than 5 mm/yr.

Falling_RSL_400

There is one more case found in the United States.  In many places in Alaska, the land is moving up at a greater rate than the sea surface is moving up (at its little 1.7 mm/yr.)  This causes the Relative Sea Level to be falling, though in reality it is the land rising faster than the surface of the sea is rising, thus the sea surface falls when measured against the shoreline.

 

 

 

Back to NOAA:

Now, back at the NOAA page for sea level rise in Montauk, NY.   At the bottom of that page, and all the other individual tide stations in this section of the site for Relative Sea Level Trends, there is a link to “Comparison of northern Atlantic station trends”.

The three images from that page have been made into the changing image shown below.

North_Atlantic_RSLR_Trends_800

What this image shows are the long-term Sea Level trends for various ports along the Eastern Seaboard of the United States.  We see that they range from 1.5 mm/yr to almost 6 mm/yr.

Does this mean that the surface of the Atlantic Ocean is rising almost three times as fast in some places along the coast as in others?   That the surface of the Atlantic is rising three times as fast at the Chesapeake Bay Tunnel (5.92 mm/yr) as in Southport, N.C. (2.01 mm/yr)?

Short Answer:  No.

The fuller answer is supplied by NOAA itself, at the top of the page that displays these charts.   NOAA states clearly:

Relative Sea Level Trends for Northern Atlantic

The graphs compare the 95% confidence intervals of relative sea level trends. Trends with the narrowest confidence intervals are based on the longest data sets. Trends with the widest confidence intervals are based on only 30-40 years of data. The graphs give an indication of the differing rates of vertical land motion, given that the absolute global sea level rise is believed to be 1.7 +/- 0.3 millimeters/year during the 20th century.

These charts (and the original graphs of Sea Level change over time at individual tide gauges) do not show how much the surface of the sea is rising (or falling) — they do not show Absolute Sea Level rise or fall.  They show Relative Sea Level Trends for individual tide gauge locations and taken together simply demonstrate visually the differing rates of vertical land motion between the stations.

It is a pleasant surprise to find that NOAA, sometimes leaning towards Sea Level Rise catastrophe advocacy, not only explains this clearly, but goes on to reiterate that “global sea level rise is believed to be 1.7 +/- 0.3 millimeters/year during the 20th century” — a figure at great variance from that promulgated by NASA, which is currently claiming to show almost twice that at  3.0 +/- 0.4 mm/yr.

NOAA makes this perfectly clear:  Tide Gauges measure Local Relative Sea Level and its changes and reflect mostly the magnitude/rate of vertical land movement..  Thus, Tide Gauges, by themselves, are not fit for the purpose of determining Global Average or Regional Average Sea Level changes, rise or fall.

Bottom Line: 

  1. Tide Gauges and tide gauge-based data can only be used to measure Local Relative Sea Level and its changes. This data is the only sea level data of importance to localities.
  2. Comparing Tide Gauge sea level trends from one tide gauge to another, as the NOAA “northern Atlantic station trends” show, only gives us “an indication of the differing rates of vertical land motion”.
  3. In order for Tide Gauges and Tide Gauge data to be useful for determining actual changes in sea surface height (or rates of change in sea surface height), regionally or globally, the Tide Gauge station must have an associated GPS@TG (GPS at tide gauge) Continuously Operating [GPS] Reference Station mounted on the same structure as the tide gauge that will precisely determine vertical movement (VLM) of the tide gauge itself.

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Author’s Comment Policy:

The topic of this post is pretty narrow:  NOAA’s statement of what a comparison of tide station sea level trends shows — “an indication of the differing rates of vertical land motion” and not rates of the rising sea surface.

I have been writing a lot about Sea Level and its changes over the last couple of years, so will be happy to try to answer your questions and refer you to sources of information.

NB:  Sea Level Rise is an ongoing  Scientific Controversy.  This means that great care must be taken in reading and interpreting the past data, new studies and especially media coverage of the topic [including this essay] — bias and advocacy are rampant, opposing forces are firing repeated salvos at one another in the journals and in the press and the consensus may well simply be “an accurate measure of the prevailing bias in the field.”  (h/t John Ioannidis)

Address your comments to “Kip…” if you are specifically looking for a response – that way I’ll see it for sure.

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March 21, 2018 4:03 am

With PDO, AMO and other oscillations, these must affect the behaviour of local air pressure which must have some significant overall affect on measured sealevel changes at any point over time.
https://www.smhi.se/en/theme/air-pressure-and-sea-level-1.12266

March 21, 2018 4:26 am

Glacial rebound plus overdrafting of aquifers makes tidal gauges unreliable in most of the US. Only tropical gauges are reliable. My favorite is Key West: no glacial rebound, no land decline issues and a long time series.

Dave
March 21, 2018 5:31 am

Kip. If one used a high number of tidal gauges from around the planet, wouldn’t the local affects tend to even out? They would still provide a useful measurement.

nobodysknowledge
March 21, 2018 5:36 am

“It is a pleasant surprise to find that NOAA, sometimes leaning towards Sea Level Rise catastrophe advocacy, not only explains this clearly, but goes on to reiterate that “global sea level rise is believed to be 1.7 +/- 0.3 millimeters/year during the 20th century” — a figure at great variance from that promulgated by NASA, which is currently claiming to show almost twice that at 3.0 +/- 0.4 mm/yr.”
Confusing statement. Presupposes that “during the 20th century” equals “currently”.
NOAA makes this perfectly clear: Tide Gauges measure Local Relative Sea Level and its changes and reflect mostly the magnitude/rate of vertical land movement.. Thus, Tide Gauges, by themselves, are not fit for the purpose of determining Global Average or Regional Average Sea Level changes, rise or fall.
Confusing statement: Strawman said that “Tide Gauges, by themselves, are fit for the purpose of determining Global Average or Regional Average Sea Level changes”. As everybody knows there is a geology of Tide Gauges, measured by GPS and estimated from many other sources.

nobodysknowledge
Reply to  nobodysknowledge
March 21, 2018 9:05 am

Is there a way to select tide gauges that can be representative of sea level change. I will chose to follow P. R. Thompson, B. D. Hamlington, F. W. Landerer, and S. Adhikari in the paper : Supporting Information for \Are long tide gauge records in the wrong place to measure global mean sea level rise?”
They are arguing in the following way. “The TG records that are most likely to represent 20th century GMSL rise satisfy the following criteria:
(1) long and mostly complete time series,
(2) located where solid earth models generally agree on the rate of sea level change due to GIA. (Perhaps solid earth models should be disqualified instead of TG records for 49 stations excluded by these criteria?)
(3) minimally affected by local, non-GIA vertical land motion.”
Then they come out with 15 TG stations: Honolulu, San Francisco, San Diego, Balboa, Christobal, Key West, Pensacola, New York, Cascais, Newlyn, Marseille, Trieste, Buenos Aires, Auckland II, and Freemantle. If we should use GPS measurements to estimate sea level rise from these stations, there are some additional problems. Balboa and Christobal don`t have GPS stations close enough to the tide gauge station. There has been recently local land subsidence at Buenos Aires and Freemantle stations, affecting GPS measurements. San Francisco GPS “not robust” because of tectonics. Auckland GPS “not robust” because groundwater variations.
So there are 9 stations left. What do they say? First we use PSMSL Tide Gauge Data to estimate local sea level change mm pr year for the years 1900 – 1999 (by Xuru linear regression). Then go into SONEL GPS data, and find vertical land movement. This give an estimate of relative SLR. And then compare it to CSIRO and ICE-6G adjustments
Honululu 1905 -1999: 1,50mm/year. GPS: -0,23 (SLR: 1,27).
CSIRO GIA: 0,34 (SLR: 1,84). Peltier ICE-6G: -0,23 (SLR: 1,27).
San Diego 1906 – 1999: 2,21mm/year, GPS: -0,99 (SLR: 1,22).
CSIRO GIA: -0,26 (SLR: 1,95). Peltier ICE-6G: -0,73 (SLR: 1,48)
Key West 1913 – 1999: 2,25mm/year. GPS: -1,07 (SLR: 1,18).
CSIRO GIA: -0,22 (SLR: 2,03). Peltier ICE-6G: -0,82 (SLR: 1,43)
Pensacola 1924 – 1999: 2,17mm/year. GPS: -0,42 (SLR: 1,75).
CSIRO GIA: -0,58 (SLR: 1,59). Peltier ICE-6G: -1,07 (SLR: 1,10)
New York 1900 – 1999: 3,00mm/year. GPS: -2,12 (SLR: 0,88).
CSIRO GIA: -0,88 (SLR: 2,12). Peltier ICE-6G: -1,80 (SLR: 1,20)
Cascais 1900 – 1993: 1,61mm/year. GPS: – 0,05 (SLR: 1,56).
CSIRO GIA: 0,05 (SLR: 1,66). Peltier ICE-6G: -0,34 (SLR: 1,27)
Newlyn 1915 – 1999: 1,65mm/year. GPS: -0,17 (SLR: 1,48).
CSIRO GIA: -0,40 (SLR: 1,25). Peltier ICE-6G: -0,72 (SLR: 0,93)
Marseille 1900 – 1999: 1,16mm/year. GPS: -0,18 (SLR: 0,98).
CSIRO GIA: -0,04 (SLR: 1,12). Peltier ICE-6G: -0,32 (SLR: 0,84)
Trieste 1901 – 1999: 1,14mm/year. GPS: 0,32 (SLR: 1,46).
CSIRO GIA: -0,03(Bar) (SLR:1,11). Peltier ICE-6G: -0,03 (SLR: 1,11)
This gives a mean rate of sea level rise of 1,31. Church and White (CSIRO) get a mean rate of sea level change of 1,63 for the same tide gauge stations, with their GIA corrections. Peltier GIA adjustments come out with a very low SLR on these stations, with mean rate of 1,18 (after changing and correcting models for 25 years).
With the same methods for the last 30 years you will get a sea level rise of over 3mm pr year. But I will argue that trends are not robust unless you use a timespan of over 60 years. Then natural variance is smoothed out.

March 21, 2018 7:38 am

The rise of sea that matters most
Is that which happens at the coast
On oceans far to west and east
Those millimetres matter least

March 21, 2018 9:44 am

Kip, it seems to me that tide gauge data is useful for a purpose in the same way that airport temperature measurements are: to provide valuable safety information to ships and planes respectively.
Neither system was intended to provide long term assessment for the change of climate variables, and neither system can do so due to too many confounding factors.
This to me is the great failure of climate scientists: failure to specify, design and implement a suitable monitoring network that could address these issues. Instead they expend huge effort on trying to coerce inappropriate measurement systems to divulge long term trends they were never designed to measure.

phil salmon
March 21, 2018 11:54 am

As the earth warms…
The real shocker here – and one with an unmistakable smoking gun of anthropogenic causation – is the above figure with SLR rates at different US coastal location. This graphic shows a correlation between rate of sea level rise and the alphabetical position of a location. Those living at locations starting with letters further up the alphabet – at no fault of their own – are imperilled by faster sea level rise and higher risk of flooding, drowning and accidental fish-swallowing.
The (we must act now) list of human activities that we now know to be linked to grievous environmental dangers and impacts just keeps on growing: now symbolic language and a written alphabet join that list of shame. Donald Trump’s persistence in sending social media tweets irresponsibly encourages people to continue and increase their use of textual communication with the Latin alphabet, which we now know to be a real risk factor for coastal flooding.
O hang on – I’m writing text in Latin alphabet now – better stop

Philip Lloyd
March 21, 2018 12:10 pm

A nice clear explanation, thanks. There is a good illustration of sinking coast according to the tide gauges all along the Gulf of Mexico to the west of the Mississippi. The land is sinking by around 6mm/year. Some suggest that it is due to water or oil abstraction, but satellite altimetry shows it is tectonic.

Philip Lloyd
Reply to  Kip Hansen
March 22, 2018 3:49 am

Yup! Most of the southern states are tilting slowly from north to south; the northern states are rising probably due to loss of ice cover; the east coast similarly appears to be sinking slowly.

March 22, 2018 1:01 am

Thank you Kip, interesting article, down here in OZ we have the most stable continent in the world.In the 1800 hundreds the British admiralty charted our coast inscribing coastal rocks with low tide lines at a particular moon phase, these show no sea level rise. Rocks out from the coast that appeared out of the water at low tide they called dry rocks and inscribed them. They are still dry rocks at low tide.
Is it only they northern oceans that are rising? Remembering that most of the worlds ocean is down here.
Regards Wayne.

March 22, 2018 4:12 pm

Hansen
Good job on sea level rise once again.
Very good gifs, although I don’t
understand why some
of them are left centric
and others are right centric,
at least on my computer.
Your writing is getting better,
not such long sentences as usual.
Of course I have to
complain about something:
On my computer — an old Apple
MacBook Pro,
the sentences and gifs
slightly overlap.
I still think you should combine
all your sea level articles
into one article of talking points
and relevant charts.
I think you have enough good
material on sea level
to create the best article of 2018
at this website —
of course I’m assuming
short, easy to read
sentences.
The more you know about a subject,
the easier it is to explain with short,
simple sentences … and you know
a lot about sea level rise.
My climate change blog
for people with common sense
— so leftists must stay away:
http://www.elOnionBloggle.Blogspot.com

Reply to  Kip Hansen
March 22, 2018 5:06 pm

Hansen:
You are hitting one home run after
another with the sea level articles.
Please do another obesity article,
so I can give you a hard time!
The zoom out feature pretty much fixed the
text / graphic overlap problem,
but the zoom in function stopped working
on my computer a few months ago,
so I was reluctant to use “zoom out” earlier —
I hope I can get back to “normal size” now.
Most people differentiate charts
by labeling them:
“Chart A”,
“Chart B”,
“Chart C”
etc.
I personally assign random numbers
to charts in my economics newsletter,
like naming the second chart “Chart 198”,
because I think that’s funny.