Sea level rise is probably the most well known impact to oceans from climate change. For those of us who live in low lying coastal areas, it has become the daily dirge we hear from environmental groups, state environmental agencies, and the media: “prepare for inundation by the ocean, prepare for inundation by the ocean.” Just last week there was yet another public talk in my town about preparing for sea level rise. It may be too late for my town; we get water in the streets every time there is a high tide. Many a time, I’ve had to wear rubber rain boots in order to get to stores and restaurants on the waterfront. It’s kind of like Venice, Italy, where residents keep their rubber boots by the door during “acqua alta.” However our problem is not simply caused by sea level rise from climate change. There are other problems accosting us, like subsidence of the whole area due to what is called isostatic rebound from former glaciers in the area. So we are getting the double whammy. We have seen almost a foot of sea level rise in the last hundred years. How do we know? Well people have been monitoring tide gauges for literally hundreds of years.
Scientists have estimated that global mean sea level has risen by 7.5 inches since 1901. They have based their estimate on records from tide gauges around the world and since 1993 on satellite data. Of course most of the tide gauge records are from Europe and North America. Did you know that the Europeans were installing and measuring tides in the 1700’s? The oldest tide gauge in the United States was installed in San Francisco Bay in 1854. There are long records of tide heights. The problem is sorting all the data so you are not seeing effects of isostatic rebound and other contributors to what scientists term “vertical land motion.” These contributors are well known in areas where there are tide gauges, and the best course of action is not to use data from areas where there is known earth movement causing the land there to rise or subside. Since the late 1990s scientists have installed global positioning receivers (i.e. GPS) near these tide gauges in order to detect the amount of vertical land motion. This will help make the data from the tide gauges useful in the future.
Very precise measurements of sea level rise have been made since the early 1990’s through the use of radar measurements from satellites orbiting the earth. Water in the oceans is constantly moving around as a result of tides, rotation of the earth, general ocean circulation, expansion and contraction from changes in temperature, the whole hydrologic cycle of evaporation, precipitation, and runoff, as well as glacier melting and formation. So sea level varies continuously. To measure the actual change in sea level rise based on the satellite data, scientists have had to build a geodetic reference frame for the earth from which the satellite radar measurements are compared. The reference frame always stays the same even if the water is moving up and down and all around. Since the measurements from the orbiting satellite are so precise, the data can be processed to determine the overall actual sea level rise versus temporary ocean changes.
So is sea level rising consistently? What is its rate of rise? According to the 2013 Intergovernmental Panel on Climate Changes (IPCC) report “The Physical Science Basis” global mean sea level has been rising at rate of .07 of an inch a year since 1901. The number is of course based on both satellite and tide gauge data over the time period. The very precise measurements from satellite data (available since 1993) show a greater rate for global mean sea level rise of .13 of an inch per year – almost double the rise calculated from the combined tide gauge and satellite data.
Sea level has been rising since the end of the last Ice Age about 14,000 years ago. There are many geologists who have made maps of the migration of the world’s coast lines over the last 14,000 years. In fact in the United States, sea level 14,000 years ago was about 300 feet lower than it is today and the coastline was nowhere near where it is now. There is a formula called “Bruns Rule” which gives you the amount of horizontal feet gained or lost per inches of sea level rise. Using the formula, I calculated that the coastline 14,000 years ago was about 5 miles from where it is now. That is a very rough estimate. There are many contributing factors that make the ratios in the Bruns Rule calculation different based on the locality. Mapping by scientists is a better way to determine exactly where the coastline was at the end of the last Ice Age. My calculation is just to give you a feel for how much distance can be covered by a change in sea level.
So what part of sea level rise is just the natural processes going on as a result of the continued interglacial epoch that we live in and what is the amount caused by humans emitting greenhouse gases? The IPCC has calculated the amount of increased heat in the upper ocean caused by human induced climate change since 1971. (See my post on temperature changes in the oceans https://waterblogger.org/general-information/increase-in-ocean-temperatures-climate-change/). Based on their calculations an average of 0.02 inches of sea level change a year has occurred as a result of the warming of the upper ocean (upper 2300 feet). Another .008 inch rise per year is a result of warming from 2300 feet to the bottom of the ocean. So roughly 0.03 inches per year of sea level rise can be attributed to greenhouse gas emissions.
Although the rate of sea level is small on a yearly basis, the rate is steady. It will eventually affect everyone who lives on the coast. And sea level rise is going to be a costly problem. I can see it happening already as my town reconstructs flood walls and puts in new drainage systems to prevent high water from flooding streets, parking lots, an