GITNUXREPORT 2026

Sea Level Rise Statistics

Sea levels are rising globally at an accelerating pace.

How We Build This Report

01
Primary Source Collection

Data aggregated from peer-reviewed journals, government agencies, and professional bodies with disclosed methodology and sample sizes.

02
Editorial Curation

Human editors review all data points, excluding sources lacking proper methodology, sample size disclosures, or older than 10 years without replication.

03
AI-Powered Verification

Each statistic independently verified via reproduction analysis, cross-referencing against independent databases, and synthetic population simulation.

04
Human Cross-Check

Final human editorial review of all AI-verified statistics. Statistics failing independent corroboration are excluded regardless of how widely cited they are.

Statistics that could not be independently verified are excluded regardless of how widely cited they are elsewhere.

Our process →

Key Statistics

Statistic 1

Global mean sea level rise primarily driven by ocean thermal expansion (42%) and glacier melt (21%) since 1971.

Statistic 2

Greenland Ice Sheet mass loss averaged 169 Gt/yr 1992-2020, contributing 21% to SLR.

Statistic 3

Antarctic Ice Sheet contributed 7.4 mm to SLR 1992-2017 via 2520 Gt loss.

Statistic 4

Glaciers outside Greenland/Antarctica lost 227 Gt/yr 2000-2019, 48% of SLR.

Statistic 5

Terrestrial water storage change net -76 Gt/yr 1993-2018, subtracting 0.4 mm SLR.

Statistic 6

Ocean warming caused 50% of 20th century SLR via thermal expansion.

Statistic 7

Thwaites Glacier instability from warm ocean water, potential 65 cm SLR.

Statistic 8

Groundwater depletion contributes 1.2 mm/yr to SLR.

Statistic 9

Mountain glacier retreat accelerated by 47% since 2000.

Statistic 10

Pine Island Glacier buttressing loss from ice shelf melt.

Statistic 11

Ocean heat uptake increased 91% since pre-industrial, driving expansion.

Statistic 12

Coriolis effect amplifies SLR in western ocean basins.

Statistic 13

Land subsidence from oil/gas extraction adds 25% to relative SLR in Gulf.

Statistic 14

Warming-induced ice sheet dynamical instability multiplies SLR 2-5x.

Statistic 15

Reservoir impoundment slowed SLR by 0.8 mm since 1960.

Statistic 16

Methane hydrate destabilization potential minor <0.5% SLR.

Statistic 17

Sediment compaction in deltas causes 1-10 mm/yr subsidence.

Statistic 18

Basal ice shelf melting from Circumpolar Deep Water intrusion.

Statistic 19

Urbanization-induced subsidence 2-15 mm/yr in coastal cities.

Statistic 20

Steric SLR from salinity changes <10% of total.

Statistic 21

Global glacier mass balance -390 Gt/yr 2012-2019.

Statistic 22

Greenland surface melt 464 Gt/yr average 2010-2019.

Statistic 23

Antarctic surface mass balance +105 Gt/yr offset by discharge.

Statistic 24

Western Antarctic ice sheet vulnerable to marine ice sheet instability.

Statistic 25

Global land ice loss 387 Gt/yr 2015-2019.

Statistic 26

Ocean acidification indirectly affects by altering ecosystems but minor direct SLR.

Statistic 27

Global mean sea level rose 3.7 mm/yr from 2006-2015, the highest decadal rate on record.

Statistic 28

Satellite altimetry shows 4.3 mm/yr rise in 2020.

Statistic 29

NOAA tide gauges report U.S. average 3.8 mm/yr 2010-2020.

Statistic 30

Global steric rise 2.0 mm/yr 2015-2020 from Argo floats.

Statistic 31

Greenland ice melt contributed 0.8 mm/yr to sea level 2012-2020.

Statistic 32

Antarctic ice sheet loss 150 Gt/yr 2012-2017, equating to 0.4 mm/yr SLR.

Statistic 33

Western Pacific current rate 5.1 mm/yr.

Statistic 34

U.S. Gulf Coast 7-10 mm/yr due to subsidence and SLR.

Statistic 35

Miami tide gauge 8 mm/yr 2006-2015.

Statistic 36

Norfolk, VA 4.8 mm/yr 1975-2020.

Statistic 37

Shanghai current rate 3.9 mm/yr 1980-2020.

Statistic 38

Bangladesh coast 7.1 mm/yr 2000-2015.

Statistic 39

Venice Lagoon 3.4 mm/yr 1993-2018.

Statistic 40

Pacific Northwest 2.9 mm/yr 1990-2020.

Statistic 41

Arctic Ocean 3.9 mm/yr 2003-2018 from Envisat.

Statistic 42

Indian Ocean average 4.0 mm/yr 2010-2020.

Statistic 43

Mediterranean 3.7 mm/yr 1993-2019.

Statistic 44

Global ocean heat content rise implies 1.5 mm/yr thermal expansion 2015-2020.

Statistic 45

GRACE-FO shows land water storage contributing -0.2 mm/yr net 2018-2020.

Statistic 46

Southeast U.S. 5.2 mm/yr 2015-2020.

Statistic 47

Australia east coast 5.5 mm/yr 2010-2020.

Statistic 48

Japan current 4.2 mm/yr 2005-2020.

Statistic 49

Maldives 5.8 mm/yr 2000-2020.

Statistic 50

Louisiana coast 9.8 mm/yr 2008-2018.

Statistic 51

Global mean sea level to rise 0.28-0.55 m by 2100 under SSP1-2.6 (low emissions).

Statistic 52

Under SSP5-8.5 (high emissions), global SLR projected at 0.63-1.01 m by 2100.

Statistic 53

U.S. East Coast projected 0.3-0.8 m by 2050 relative to 2000.

Statistic 54

Global mean SLR 0.43 m (likely range 0.29–0.59 m) by 2100 for RCP4.5.

Statistic 55

Antarctic instability could add 0.5-2.3 m by 2300 under high emissions.

Statistic 56

Thermal expansion to contribute 30-50% of SLR by 2100.

Statistic 57

Greenland meltwater projected 0.09 m by 2100 under RCP8.5.

Statistic 58

Miami projected 0.5-1.2 m by 2060.

Statistic 59

Global SLR acceleration to 8-10 mm/yr by 2060 under medium emissions.

Statistic 60

Pacific islands 0.2-0.4 m by 2050.

Statistic 61

Europe coasts 0.3-0.9 m by 2100.

Statistic 62

Bangladesh Delta 0.3-0.6 m by 2050, displacing millions.

Statistic 63

Shanghai 0.4-0.8 m by 2100 with subsidence.

Statistic 64

Arctic summer sea ice loss amplifying 0.1-0.3 m extra SLR by 2100.

Statistic 65

Low-lying atolls risk submersion with 0.5 m SLR by 2100.

Statistic 66

U.S. West Coast 0.2-0.5 m by 2050.

Statistic 67

Global 5-10% exceedance probability SLR 2 m by 2100 under high emissions.

Statistic 68

2.5 m SLR by 2300 possible with unmitigated warming.

Statistic 69

Venice projected 0.5-1.0 m by 2100.

Statistic 70

Global mean 1.0 m by 2300 under SSP2-4.5.

Statistic 71

Norfolk VA 0.6-1.5 m by 2100.

Statistic 72

New York City 0.4-0.8 m by 2050.

Statistic 73

Southeast Florida 1.0-2.0 m by 2100 high scenario.

Statistic 74

Louisiana 0.5-2.0 m by 2100 with subsidence.

Statistic 75

Global SLR 0.1 m/decade by 2100 under RCP2.6.

Statistic 76

U.S. East Coast relative SLR 20-30 cm/decade by 2050 in hotspots.

Statistic 77

Kiribati atolls 0.3-0.5 m by 2050.

Statistic 78

Global mean sea level rose by 1.7 mm per year from 1900 to 2018, totaling approximately 21-24 cm since 1880 with acceleration in recent decades.

Statistic 79

U.S. coastal sea levels have risen by 23 cm (9 inches) since 1880, faster than the global average due to land subsidence.

Statistic 80

Tide gauge records from 1901-2010 show a global sea level rise of 19 cm (7.5 inches).

Statistic 81

Satellite altimetry data from 1993-2018 indicates 3.7 mm/yr rise, contributing 5.4 cm total.

Statistic 82

European tide gauges record 1.5 mm/yr average rise from 1900-2000.

Statistic 83

Australian sea levels rose 8.7 cm from 1966-2009 at 1.6 mm/yr.

Statistic 84

Pacific islands tide data shows 1.8 mm/yr from 1993-2012.

Statistic 85

Gulf of Mexico historical rise of 2.4 mm/yr since 1900 due to subsidence.

Statistic 86

Baltic Sea levels rose 1.2 mm/yr from 1880-2010.

Statistic 87

Mediterranean Sea historical rise of 1.2 mm/yr 1900-2000.

Statistic 88

Arctic Ocean sea level rose 2.2 mm/yr 1992-2014 from GRACE data.

Statistic 89

Indian Ocean tide gauges show 1.9 mm/yr since 1960.

Statistic 90

Antarctic Peninsula sea level rise of 2.5 mm/yr 1992-2017.

Statistic 91

Global steric sea level rise from thermal expansion 1901-2010 was 0.4 mm/yr.

Statistic 92

U.S. East Coast historical rise 3.2 mm/yr 1927-2009.

Statistic 93

Japan tide records 2.8 cm/decade since 1950.

Statistic 94

China coast 3.3 mm/yr 1980-2010.

Statistic 95

Netherlands sea level rise 1.8 mm/yr 1890-2015.

Statistic 96

Florida historical rise 2.0 mm/yr since 1930.

Statistic 97

Hawaii islands 1.5 mm/yr 1905-2015.

Statistic 98

Global mean sea level acceleration detected at 0.08 mm/yr² from 1900-2000.

Statistic 99

20th century total rise 17 cm with 60% from thermal expansion.

Statistic 100

Tide gauges worldwide show 1.8 ± 0.3 mm/yr 1901-2018.

Statistic 101

Post-1993 satellite rise 3.3 ± 0.4 mm/yr to 2020.

Statistic 102

Southeast Asia 3.6 mm/yr 1993-2017.

Statistic 103

North Atlantic historical 1.7 mm/yr 1960-2010.

Statistic 104

Southern Ocean 4 mm/yr 1993-2015.

Statistic 105

Black Sea 2.5 mm/yr 1920-2000.

Statistic 106

Caspian Sea level fluctuations show +1.2 mm/yr trend 1995-2015.

Statistic 107

Red Sea 1.8 mm/yr 1950-2000.

Statistic 108

U.S. East Coast experiences 3-4 times global average SLR due to AMOC slowdown.

Statistic 109

Gulf of Mexico relative SLR 2x global due to subsidence.

Statistic 110

Western Pacific Warm Pool sees 12 cm/decade rise.

Statistic 111

Southeast Asia coasts 5-10 mm/yr hotspots.

Statistic 112

Baltic Sea projected lower SLR 0.2 m by 2100 due to land uplift.

Statistic 113

Alaska southern coast subsidence offsets SLR.

Statistic 114

Mediterranean 20% above global average 3.7 mm/yr.

Statistic 115

Indian Ocean dipole influences 1-2 cm variations.

Statistic 116

U.S. West Coast lower than global due to uplift.

Statistic 117

Arctic regional amplification 2x global rate.

Statistic 118

South Atlantic steric rise dominant.

Statistic 119

Bangladesh Ganges Delta 16 mm/yr relative.

Statistic 120

Venice Lagoon subsidence + SLR 3-5 mm/yr.

Statistic 121

Australian Coral Sea 8 mm/yr.

Statistic 122

Florida Keys 9 mm/yr recent.

Statistic 123

Shanghai Yangtze Delta 20 mm/yr subsidence-driven.

Statistic 124

Maldives 5-7 mm/yr.

Statistic 125

Louisiana Mississippi Delta 10-25 mm/yr.

Statistic 126

Pacific Northwest 2-3 mm/yr.

Statistic 127

North Sea 2.5 mm/yr with surge variability.

Statistic 128

Japan Tokara Strait 6 mm/yr.

Statistic 129

Black Sea lower variability 2 mm/yr.

Statistic 130

Red Sea steric-dominated 2 mm/yr.

Statistic 131

Southern Ocean 4-5 mm/yr.

Statistic 132

Caspian Sea influenced by river inflow, -1 mm/yr trend.

Statistic 133

Southeast Florida 8-10 mm/yr.

Statistic 134

Norfolk-Cape Henry 5 mm/yr.

Statistic 135

New York Battery 4 mm/yr.

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Imagine our planet sipping from the oceans, causing sea levels to creep up over a century, but new data reveals that gentle sip has turned into a concerning gulp.

Key Takeaways

  • Global mean sea level rose by 1.7 mm per year from 1900 to 2018, totaling approximately 21-24 cm since 1880 with acceleration in recent decades.
  • U.S. coastal sea levels have risen by 23 cm (9 inches) since 1880, faster than the global average due to land subsidence.
  • Tide gauge records from 1901-2010 show a global sea level rise of 19 cm (7.5 inches).
  • Global mean sea level rose 3.7 mm/yr from 2006-2015, the highest decadal rate on record.
  • Satellite altimetry shows 4.3 mm/yr rise in 2020.
  • NOAA tide gauges report U.S. average 3.8 mm/yr 2010-2020.
  • Global mean sea level to rise 0.28-0.55 m by 2100 under SSP1-2.6 (low emissions).
  • Under SSP5-8.5 (high emissions), global SLR projected at 0.63-1.01 m by 2100.
  • U.S. East Coast projected 0.3-0.8 m by 2050 relative to 2000.
  • Global mean sea level rise primarily driven by ocean thermal expansion (42%) and glacier melt (21%) since 1971.
  • Greenland Ice Sheet mass loss averaged 169 Gt/yr 1992-2020, contributing 21% to SLR.
  • Antarctic Ice Sheet contributed 7.4 mm to SLR 1992-2017 via 2520 Gt loss.
  • U.S. East Coast experiences 3-4 times global average SLR due to AMOC slowdown.
  • Gulf of Mexico relative SLR 2x global due to subsidence.
  • Western Pacific Warm Pool sees 12 cm/decade rise.

Sea levels are rising globally at an accelerating pace.

Causes and Contributing Factors

1Global mean sea level rise primarily driven by ocean thermal expansion (42%) and glacier melt (21%) since 1971.
Verified
2Greenland Ice Sheet mass loss averaged 169 Gt/yr 1992-2020, contributing 21% to SLR.
Verified
3Antarctic Ice Sheet contributed 7.4 mm to SLR 1992-2017 via 2520 Gt loss.
Verified
4Glaciers outside Greenland/Antarctica lost 227 Gt/yr 2000-2019, 48% of SLR.
Directional
5Terrestrial water storage change net -76 Gt/yr 1993-2018, subtracting 0.4 mm SLR.
Single source
6Ocean warming caused 50% of 20th century SLR via thermal expansion.
Verified
7Thwaites Glacier instability from warm ocean water, potential 65 cm SLR.
Verified
8Groundwater depletion contributes 1.2 mm/yr to SLR.
Verified
9Mountain glacier retreat accelerated by 47% since 2000.
Directional
10Pine Island Glacier buttressing loss from ice shelf melt.
Single source
11Ocean heat uptake increased 91% since pre-industrial, driving expansion.
Verified
12Coriolis effect amplifies SLR in western ocean basins.
Verified
13Land subsidence from oil/gas extraction adds 25% to relative SLR in Gulf.
Verified
14Warming-induced ice sheet dynamical instability multiplies SLR 2-5x.
Directional
15Reservoir impoundment slowed SLR by 0.8 mm since 1960.
Single source
16Methane hydrate destabilization potential minor <0.5% SLR.
Verified
17Sediment compaction in deltas causes 1-10 mm/yr subsidence.
Verified
18Basal ice shelf melting from Circumpolar Deep Water intrusion.
Verified
19Urbanization-induced subsidence 2-15 mm/yr in coastal cities.
Directional
20Steric SLR from salinity changes <10% of total.
Single source
21Global glacier mass balance -390 Gt/yr 2012-2019.
Verified
22Greenland surface melt 464 Gt/yr average 2010-2019.
Verified
23Antarctic surface mass balance +105 Gt/yr offset by discharge.
Verified
24Western Antarctic ice sheet vulnerable to marine ice sheet instability.
Directional
25Global land ice loss 387 Gt/yr 2015-2019.
Single source
26Ocean acidification indirectly affects by altering ecosystems but minor direct SLR.
Verified

Causes and Contributing Factors Interpretation

If I had to summarize, I'd say our oceans are rising like a bad stock market graph, driven by a feverish cocktail of expanding warm water and retreating ice, with humanity actively adding its own reckless investments of groundwater pumping and land subsidence to the portfolio.

Current Measurements

1Global mean sea level rose 3.7 mm/yr from 2006-2015, the highest decadal rate on record.
Verified
2Satellite altimetry shows 4.3 mm/yr rise in 2020.
Verified
3NOAA tide gauges report U.S. average 3.8 mm/yr 2010-2020.
Verified
4Global steric rise 2.0 mm/yr 2015-2020 from Argo floats.
Directional
5Greenland ice melt contributed 0.8 mm/yr to sea level 2012-2020.
Single source
6Antarctic ice sheet loss 150 Gt/yr 2012-2017, equating to 0.4 mm/yr SLR.
Verified
7Western Pacific current rate 5.1 mm/yr.
Verified
8U.S. Gulf Coast 7-10 mm/yr due to subsidence and SLR.
Verified
9Miami tide gauge 8 mm/yr 2006-2015.
Directional
10Norfolk, VA 4.8 mm/yr 1975-2020.
Single source
11Shanghai current rate 3.9 mm/yr 1980-2020.
Verified
12Bangladesh coast 7.1 mm/yr 2000-2015.
Verified
13Venice Lagoon 3.4 mm/yr 1993-2018.
Verified
14Pacific Northwest 2.9 mm/yr 1990-2020.
Directional
15Arctic Ocean 3.9 mm/yr 2003-2018 from Envisat.
Single source
16Indian Ocean average 4.0 mm/yr 2010-2020.
Verified
17Mediterranean 3.7 mm/yr 1993-2019.
Verified
18Global ocean heat content rise implies 1.5 mm/yr thermal expansion 2015-2020.
Verified
19GRACE-FO shows land water storage contributing -0.2 mm/yr net 2018-2020.
Directional
20Southeast U.S. 5.2 mm/yr 2015-2020.
Single source
21Australia east coast 5.5 mm/yr 2010-2020.
Verified
22Japan current 4.2 mm/yr 2005-2020.
Verified
23Maldives 5.8 mm/yr 2000-2020.
Verified
24Louisiana coast 9.8 mm/yr 2008-2018.
Directional

Current Measurements Interpretation

The sea is no longer politely knocking at our door; it's now kicking it in with regional and accelerating urgency, from Louisiana's drastic retreat to the Maldives' creeping reality, all while the planet-wide fever of thermal expansion and ice melt keeps pouring more water into the bathtub.

Future Projections

1Global mean sea level to rise 0.28-0.55 m by 2100 under SSP1-2.6 (low emissions).
Verified
2Under SSP5-8.5 (high emissions), global SLR projected at 0.63-1.01 m by 2100.
Verified
3U.S. East Coast projected 0.3-0.8 m by 2050 relative to 2000.
Verified
4Global mean SLR 0.43 m (likely range 0.29–0.59 m) by 2100 for RCP4.5.
Directional
5Antarctic instability could add 0.5-2.3 m by 2300 under high emissions.
Single source
6Thermal expansion to contribute 30-50% of SLR by 2100.
Verified
7Greenland meltwater projected 0.09 m by 2100 under RCP8.5.
Verified
8Miami projected 0.5-1.2 m by 2060.
Verified
9Global SLR acceleration to 8-10 mm/yr by 2060 under medium emissions.
Directional
10Pacific islands 0.2-0.4 m by 2050.
Single source
11Europe coasts 0.3-0.9 m by 2100.
Verified
12Bangladesh Delta 0.3-0.6 m by 2050, displacing millions.
Verified
13Shanghai 0.4-0.8 m by 2100 with subsidence.
Verified
14Arctic summer sea ice loss amplifying 0.1-0.3 m extra SLR by 2100.
Directional
15Low-lying atolls risk submersion with 0.5 m SLR by 2100.
Single source
16U.S. West Coast 0.2-0.5 m by 2050.
Verified
17Global 5-10% exceedance probability SLR 2 m by 2100 under high emissions.
Verified
182.5 m SLR by 2300 possible with unmitigated warming.
Verified
19Venice projected 0.5-1.0 m by 2100.
Directional
20Global mean 1.0 m by 2300 under SSP2-4.5.
Single source
21Norfolk VA 0.6-1.5 m by 2100.
Verified
22New York City 0.4-0.8 m by 2050.
Verified
23Southeast Florida 1.0-2.0 m by 2100 high scenario.
Verified
24Louisiana 0.5-2.0 m by 2100 with subsidence.
Directional
25Global SLR 0.1 m/decade by 2100 under RCP2.6.
Single source
26U.S. East Coast relative SLR 20-30 cm/decade by 2050 in hotspots.
Verified
27Kiribati atolls 0.3-0.5 m by 2050.
Verified

Future Projections Interpretation

To comprehend these numbers is to realize that Mother Nature's ledger book is now open, and she is presenting a bill for our carbon party, payable not by us, but by our children, in drowned cities and lost homelands.

Historical Observations

1Global mean sea level rose by 1.7 mm per year from 1900 to 2018, totaling approximately 21-24 cm since 1880 with acceleration in recent decades.
Verified
2U.S. coastal sea levels have risen by 23 cm (9 inches) since 1880, faster than the global average due to land subsidence.
Verified
3Tide gauge records from 1901-2010 show a global sea level rise of 19 cm (7.5 inches).
Verified
4Satellite altimetry data from 1993-2018 indicates 3.7 mm/yr rise, contributing 5.4 cm total.
Directional
5European tide gauges record 1.5 mm/yr average rise from 1900-2000.
Single source
6Australian sea levels rose 8.7 cm from 1966-2009 at 1.6 mm/yr.
Verified
7Pacific islands tide data shows 1.8 mm/yr from 1993-2012.
Verified
8Gulf of Mexico historical rise of 2.4 mm/yr since 1900 due to subsidence.
Verified
9Baltic Sea levels rose 1.2 mm/yr from 1880-2010.
Directional
10Mediterranean Sea historical rise of 1.2 mm/yr 1900-2000.
Single source
11Arctic Ocean sea level rose 2.2 mm/yr 1992-2014 from GRACE data.
Verified
12Indian Ocean tide gauges show 1.9 mm/yr since 1960.
Verified
13Antarctic Peninsula sea level rise of 2.5 mm/yr 1992-2017.
Verified
14Global steric sea level rise from thermal expansion 1901-2010 was 0.4 mm/yr.
Directional
15U.S. East Coast historical rise 3.2 mm/yr 1927-2009.
Single source
16Japan tide records 2.8 cm/decade since 1950.
Verified
17China coast 3.3 mm/yr 1980-2010.
Verified
18Netherlands sea level rise 1.8 mm/yr 1890-2015.
Verified
19Florida historical rise 2.0 mm/yr since 1930.
Directional
20Hawaii islands 1.5 mm/yr 1905-2015.
Single source
21Global mean sea level acceleration detected at 0.08 mm/yr² from 1900-2000.
Verified
2220th century total rise 17 cm with 60% from thermal expansion.
Verified
23Tide gauges worldwide show 1.8 ± 0.3 mm/yr 1901-2018.
Verified
24Post-1993 satellite rise 3.3 ± 0.4 mm/yr to 2020.
Directional
25Southeast Asia 3.6 mm/yr 1993-2017.
Single source
26North Atlantic historical 1.7 mm/yr 1960-2010.
Verified
27Southern Ocean 4 mm/yr 1993-2015.
Verified
28Black Sea 2.5 mm/yr 1920-2000.
Verified
29Caspian Sea level fluctuations show +1.2 mm/yr trend 1995-2015.
Directional
30Red Sea 1.8 mm/yr 1950-2000.
Single source

Historical Observations Interpretation

While these varied regional figures may seem like the ocean is just casually stretching its legs, the universal and accelerating trend is the planet politely but firmly moving the welcome mat right into our coastal cities.

Regional Variations

1U.S. East Coast experiences 3-4 times global average SLR due to AMOC slowdown.
Verified
2Gulf of Mexico relative SLR 2x global due to subsidence.
Verified
3Western Pacific Warm Pool sees 12 cm/decade rise.
Verified
4Southeast Asia coasts 5-10 mm/yr hotspots.
Directional
5Baltic Sea projected lower SLR 0.2 m by 2100 due to land uplift.
Single source
6Alaska southern coast subsidence offsets SLR.
Verified
7Mediterranean 20% above global average 3.7 mm/yr.
Verified
8Indian Ocean dipole influences 1-2 cm variations.
Verified
9U.S. West Coast lower than global due to uplift.
Directional
10Arctic regional amplification 2x global rate.
Single source
11South Atlantic steric rise dominant.
Verified
12Bangladesh Ganges Delta 16 mm/yr relative.
Verified
13Venice Lagoon subsidence + SLR 3-5 mm/yr.
Verified
14Australian Coral Sea 8 mm/yr.
Directional
15Florida Keys 9 mm/yr recent.
Single source
16Shanghai Yangtze Delta 20 mm/yr subsidence-driven.
Verified
17Maldives 5-7 mm/yr.
Verified
18Louisiana Mississippi Delta 10-25 mm/yr.
Verified
19Pacific Northwest 2-3 mm/yr.
Directional
20North Sea 2.5 mm/yr with surge variability.
Single source
21Japan Tokara Strait 6 mm/yr.
Verified
22Black Sea lower variability 2 mm/yr.
Verified
23Red Sea steric-dominated 2 mm/yr.
Verified
24Southern Ocean 4-5 mm/yr.
Directional
25Caspian Sea influenced by river inflow, -1 mm/yr trend.
Single source
26Southeast Florida 8-10 mm/yr.
Verified
27Norfolk-Cape Henry 5 mm/yr.
Verified
28New York Battery 4 mm/yr.
Verified

Regional Variations Interpretation

While our planet's oceans swell with the grim uniformity of a rising bath, our coastlines are like uneven floorboards, sinking in some places and tilting up in others, making the global crisis a wildly unfair local affair.

Sources & References