Table 11.9 of the TAR listed several estimates for global and regional 20th - century
sea level trends based on the Permanent Service for Mean Sea Level (PSMSL) data set (Woodworth and Player, 2003).
The map of regional mean sea level trends provides an overview of variations in the rates of relative local mean sea level observed at long - term tide stations (based on a minimum of 30 years of data in order to account for long - term sea level variations and reduce errors in computing
sea level trends based on monthly mean sea level).
Not exact matches
After over a year of sideways and downward movement from late 2015 through early 2017, the most recent NASA report shows that over the past year an acceleration in
sea level rise has become visible on the NASA graph, even with just a quick glance (then again, while the long term
trend is consistently upward, the annual
trend is so variable, that it's likely foolish on my part to suggest a change in
trend based on the most recent periods of increase which have only been occurring for less than 12 months).
Canadian Ice Service, 4.7, Multiple Methods As with CIS contributions in June 2009, 2010, and 2011, the 2012 forecast was derived using a combination of three methods: 1) a qualitative heuristic method
based on observed end - of - winter arctic ice thicknesses and extents, as well as an examination of Surface Air Temperature (SAT), Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model, which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predic
based on observed end - of - winter arctic ice thicknesses and extents, as well as an examination of Surface Air Temperature (SAT),
Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model, which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
Sea Level Pressure (SLP) and vector wind anomaly patterns and
trends; 2) an experimental Optimal Filtering
Based (OFB) Model, which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predic
Based (OFB) Model, which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and
sea ice predicto
sea ice predictors.
Canadian Ice Service, 4.7 (+ / - 0.2), Heuristic / Statistical (same as June) The 2015 forecast was derived by considering a combination of methods: 1) a qualitative heuristic method
based on observed end - of - winter Arctic ice thickness extents, as well as winter Surface Air Temperature, Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predic
based on observed end - of - winter Arctic ice thickness extents, as well as winter Surface Air Temperature,
Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
Sea Level Pressure and vector wind anomaly patterns and
trends; 2) a simple statistical method, Optimal Filtering
Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predic
Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September
sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and
sea ice predicto
sea ice predictors.
Raw satellite -
based trends in global mean
sea levels over the period 1992 - 2000, according to Morner, 2004.
John Church, a top IPCC author at the Commonwealth Scientific and Industrial Research Organization in Australia, told Reuters he did not expect any impact on the IPCC's core
sea level projections, which are not
based on past
trends.
The Harvard - led study said the new findings might affect projections of the future pace of
sea level rise, especially those
based on historical
trends.
We also compared how the observed number of nuisance flood days in 2014 compared to what would be expected
based on
sea level rise
trends in each location.
Finally, we project the number of nuisance flood days that we would expect from May 2015 - April 2016
based on
sea level trends trends alone and with the added influence of El Niño.
Combine the satellite
trend with the surface observations and the umpteen non-temperature
based records that reflect temperature change (from glaciers to phenology to lake freeze dates to snow - cover extent in spring & fall to
sea level rise to stratospheric temps) and the evidence for recent gradual warming is, well, unequivocal.
Since current ice melt data could indicate variable climate
trends and aren't necessarily part of an accelerating
trend, the study warned that predictions of future
sea -
level rise should not be
based on measurements of glacial loss» Daily Mail.
Canadian Ice Service; 5.0; Statistical As with Canadian Ice Service (CIS) contributions in June 2009 and June 2010, the 2011 forecast was derived using a combination of three methods: 1) a qualitative heuristic method
based on observed end - of - winter Arctic Multi-Year Ice (MYI) extents, as well as an examination of Surface Air Temperature (SAT), Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere, and sea ice predic
based on observed end - of - winter Arctic Multi-Year Ice (MYI) extents, as well as an examination of Surface Air Temperature (SAT),
Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere, and sea ice predicto
Sea Level Pressure (SLP) and vector wind anomaly patterns and
trends; 2) an experimental Optimal Filtering
Based (OFB) Model which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere, and sea ice predic
Based (OFB) Model which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere, and
sea ice predicto
sea ice predictors.
IPCC synthesis reports offer conservative projections of
sea level increase
based on assumptions about future behavior of ice sheets and glaciers, leading to estimates of
sea level roughly following a linear upward
trend mimicking that of recent decades.
Canadian Ice Service, 4.7 (± 0.2), Heuristic / Statistical (same as June) The 2015 forecast was derived by considering a combination of methods: 1) a qualitative heuristic method
based on observed end - of - winter Arctic ice thickness extents, as well as winter Surface Air Temperature, Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predic
based on observed end - of - winter Arctic ice thickness extents, as well as winter Surface Air Temperature,
Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
Sea Level Pressure and vector wind anomaly patterns and
trends; 2) a simple statistical method, Optimal Filtering
Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predic
Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September
sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and
sea ice predicto
sea ice predictors.
It remains possible that the data
base is insufficient to compute mean
sea level trends with the accuracy necessary to discuss the impact of global warming — as disappointing as this conclusion may be.
The increase in the rate of
sea level rise at Stockholm (the longest record that extends past 1900) has been
based on differencing 100 - year
trends from 1774 — 1884 and 1885 — 1985.
Although the calculations of 18 - year rates of GMSL rise
based on the different reconstruction methods disagree by as much as 2 mm mm yr - 1 before 1950 and on details of the variability (Figure 3.14), all do indicate 18 - year
trends that were significantly higher than the 20th century average at certain times (1920 — 1950, 1990 — present) and lower at other periods (1910 — 1920, 1955 — 1980), likely related to multidecadal variability.The IPCC AR5 found that it is likely that a
sea level rise rate comparable to that since 1993 occurred between 1920 and 1950.
Notes: Excel was used to calculate and plot the moving
sea level per century curves and fitted
trends (Excel slope function produced
trends based on moving 360 - month periods for each month in the dataset; then converted to per century
trends (inches) for each month).
In this context, we develop national projections of the urban and non-urban coastal population on the
basis of four environmental and socio - economic scenarios which account for
sea -
level rise (for the flood plain analysis), population distribution,
trends in urbanisation and coastal population growth.
See E.W. Leuliette, R.S. Nerem, and G.T. Mitchum, «Results of TOPEX / Poseidon and Jason - 1 calibration to construct a continuous record of mean
sea level,» Marine Geodesy 27:79 - 94, 2004, and B.D. Beckley, F.G. Lemoine, S.B. Luthcke, R.D. Ray, and N.P. Zelensky, «A reassessment of global and regional mean
sea level trends from TOPEX and Jason - 1 altimetry
based on revised reference frame and orbits,» Geophysical Research Letters 34 (14): L14608, 2007.
Yes, the first Table (Recent short - term
sea level trends in the Project area
based upon SEAFRAME data through September 2006) lists
trends of 2.7 to 17 mm / yr.
This expansion, combined with the melting of land -
based ice, has caused global average
sea level to rise by roughly 7 - 8 inches since 1900 — a
trend that is expected to accelerate over coming decades.