Houston’s (and Galveston’s) High Water Problems

Saturday, December 27, 2008

Houston’s High Water Problems

The following article is found at www.thehoustonlawyer.com (http://www.thehoustonlawyer.com/aa_nov08/page18.htm)

Houston’s High Water Problems

By Jim Blackburn and Larry Dunbar

We as a community stand in the aftermath of Hurricane Ike. To say that Ike swept us away is a gross understatement. Some on the Texas Gulf Coast felt Ike’s presence with high tide and flooding occurring before the storm made landfall. Those who never met Hurricane Alicia could not believe their eyes. Although damage from flooding is undeniably evident, determining causation liability is more difficult. Separated by few determining factors, legal issues in flooding and drainage require expertise in local, state and federal case law and are not limited to statutory or common law claims. The following is but an overview of drainage and flooding issues in Houston, the current situation and a glimpse of where we may be heading. To do justice to this subject would require much more space than is available here.

Flooding is Not a New Issue

Flooding and drainage have always been problems in Houston. Settlers traveling through Houston in the mid to late 1800s reported walking for days west of town in ankle to knee-deep water. Downtown Houston was flooded in the 1930s by Buffalo Bayou, leading to the construction of Addicks and Barker Reservoirs by the Corps of Engineers. These two flood control reservoirs are arguably the best flood control money ever spent in this flat coastal terrain.

Applicable Laws, Regulations, and Programs

Harris County Flood Control District (HCFCD) was created in 1937 by the Texas Legislature originally to be a local partner with the Federal Corps of Engineers for these two flood control reservoirs and other flood control projects in and around Houston. The District was also given responsibility for managing our local waterways “for domestic, municipal, flood control, irrigation and other useful purposes.” This important responsibility will be referenced later.

The basic drainage statute is Section 11.086 of the Texas Water Code, which codifies Spanish law that the overland flow of surface water before it enters a watercourse cannot be redirected and/or increased on downstream properties or thrown back on upstream properties. This section is interpreted as a strict liability statute to be used against landowners for their development activities that alter drainage and cause damage to nearby properties. Statutes relating to watercourses apply once the surface water enters a watercourse (a stream with a defined bed and banks). Although Texans are not supposed to increase the stormwater runoff that flows overland and into the watercourses, extensive development in and around Houston did just that.

In addition to common law and statutory rights to take legal action for flood damages already incurred, governmental regulation and other actions play a major role in preventing development activity from causing undue flood damage. The National Flood Insurance Program provides flood insurance for residents of communities that implement land use controls for high hazard areas based on flood plain maps. Today, virtually all cities and counties on the Texas Coast participate in this federal program, and flood plain maps (and their implications) are part of common parlance in real estate development. Similarly, drainage is regulated by many counties and cities in an attempt to minimize damages due to flooding from land development. There is no question that the placement of concrete and the construction of drainage channels in the flat Texas coast can and does increase stormwater runoff, notwithstanding the prohibitions of Section 11.086 of the Texas Water Code.3

Today in Harris County and certain surrounding counties, we live with the damaging by-product of decades of suburban development. Our flood plains are increasing in size, primarily as a result of upstream development that increases downstream flows and the corresponding flooding. Some homeowners today are in the 100-year flood plain or floodway, even though their same properties are not so shown on prior flood plain maps. Others simply find themselves flooded when they thought they were high and dry. All ask an obvious question:

What Happened?

1. The Size of Houston’s Floodplain Grew as Houston Grew A review of historical flood plain maps show how Houston’s flood plain has increased in size over time. Nowhere is this more evident than on White Oak Bayou where significant changes occurred in the 100-year flood plain map since 1996. In 1996, only 4354 acres were in the 100-year flood plain. By 2007, that number doubled to 9617 acres. Similarly, the size of the 100-year floodway grew from 2073 acres in 1996 to 3337 acres in 2007. For the most part, the floodplain and floodway increases occurred within already-developed areas. For example, the floodplain now is about one mile wide inside Loop 610 whereas it previously was restricted to a small area along the channel.

Today there is major litigation in Harris County regarding drainage and flooding that will affect all of us. Here is a short summary of certain key cases and issues.

a. The Kerr Case

Kerr v. Harris County is currently pending in County Court at Law No.1.4 This case has twice been ruled upon by the 14th Court of Appeals, once on issues of law and causation, and once on a plea to the jurisdiction that led to the case being refiled in county court rather than district court due to a change in legislative jurisdiction determined after the filing of the original case.5Kerr is based on Article I, Section 17 of the Texas Constitution, claiming inverse condemnation – the homes were taken by Harris County and used for flood storage. Rather than construct a regional flood control plan adopted for the White Oak Bayou Watershed in the late 1980s, the plaintiffs in Kerr allege that Harris County chose not to build critical components of the plan because it found itself short of money. Moreover, developers were allowed to pay money to Harris County in lieu of building on-site detention ponds; thereby allowing additional runoff from upstream development to flow unmitigated downstream into a bayou the county knew had no capacity to handle any more water. The plaintiffs’ claim that Harris County essentially rolled the dice that sufficient funds would be available to complete the project before any big rains came along. Unfortunately, downstream homeowners’ properties were flooded when the county lost the bet, not only in 1998 but also in 2001 – and again in 2002. Because of the county’s choice, the plaintiffs argue that downstream properties of those living adjacent to the bayou, but out of the flood plain, were used to store those additional flood waters.

Kerr has generated substantial defense theories, many of which were rendered moot. The initial lawsuit was challenged on the basis that a permanent taking cannot be generated by a single flood event (although constitutional damaging might be). However, the occurrence of two subsequent flood events that damaged most of the same homes rendered that defense moot. Other defense theories such as Act of God – e.g., the rainfall amount was unprecedented – have been dropped in subsequent admissions and/or responses to interrogatories. The case now comes down to whether the intentional failure of Harris County to construct the regional flood control plan with its substantially certain consequences of downstream flooding will be found the primary cause of damages suffered by the flooded residents.

This case is headed to trial in early 2009. For over nine years, no jury has heard these claims. This is due at least in part to the operation of the Plea to the Jurisdiction, a judicial tool that appears to deny plaintiffs the right to a speedy trial when they sue the government.

It is interesting to note that the change in the extent of flooding along White Oak Bayou first raised in Kerr in 1999 is now ratified by recent changes in the official flood plain map. Although the citizens included in the Kerr litigation may have a chance for compensation, many other downstream residents now find themselves in areas labeled “flood-prone” with no available compensation for damages.

2. Flood Plain Maps Are Not Accurate

The concept behind flood plain regulations is that risks inherent in the development of certain high hazard areas are identified on flood plain maps and then regulations are passed to insure the safety of housing and other developments to be located in such areas. The flood plain regulations are based on maps that delineate the 100-year flood plain – the area flooded by a storm recurring once every 100 years, and the 100-year floodway – the area within the flood plain where most of the water actually flows. Under the federal program, development is allowed within the 100-year flood plain outside of the 100-year floodway if minimum slab elevation restrictions are met. More restrictive regulations apply to development within the 100-year floodway.

It is extremely important that the flood plain maps for the community are accurate. After tropical storms Frances and Allison, major efforts were taken to redo the Harris County flood plain maps due to obvious inaccuracies. The results of the remapping can be seen at the web site http://www.tsarp.org/. These flood plain revisions clearly show the increased amount of area now within the 100-year flood plain and 100-year floodway in Harris County, particularly on White Oak Bayou from Beltway 8 eastward through the Houston Heights to downtown.

Several issues were raised over the accuracy of these new flood plain maps. The publication of flood plain maps takes place under the auspices of the Federal Emergency Management Agency (FEMA) as an administrative law process under the federal Administrative Procedure Act. Notice of the availability of draft flood plain maps is published in the Federal Register. Opportunity is provided for public review and comment. Anyone wishing to complain about the accuracy of a flood plain map must submit written comments or file an appeal. FEMA takes the position that a request for a change in the draft map must also be accompanied by technical computer modeling demonstrating the error of the proposed maps. This task is so financially daunting that individual property owners and most homeowner associations, by default, lack a voice in the process.

a. The Sierra Club Case

Key litigation over inaccurate flood plain mapping and the commenting process was recently filed in federal court in Houston. Sierra Club v. FEMA, et al., filed in 2007, is pending in Judge Lee Rosenthal’s court.6 This case arises over the remapping of the flood plain for Cypress Creek, a major watercourse that rises in Waller County, meanders southeast and then northward, ultimately flowing easterly across northern Harris County where it empties into the San Jacinto River and Lake Houston. The area of concern in the litigation is in the upper portion of the watershed, west of the U.S. 290 crossing of Cypress Creek in the Katy Prairie.

Although the Sierra Club brought this lawsuit, several other parties, including Houston Voters Against Flooding (HVAF) and the Cypress Creek Flood Control Coalition (CCFCC), submitted comments on the Draft map. The basic contention is that the flood plain elevation depicted on the flood plain maps along Upper Cypress Creek is as much as four feet too low. There have been at least two storms in the last ten years that were less than 100-year rain events and generated flood flows measuring four feet higher than the revised map indicated along Cypress Creek at the gauge at Katy Hockley Road. The Sierra Club was concerned about this identified error because development could occur in areas of the Katy Prairie without being subject to flood plain rules and federal wetland rules (due to a linkage between federal wetland jurisdiction and flood plain maps). The Cypress Creek Flood Control Coalition was concerned that the computer modeling used to create these flood plain maps showed too much water flowing downstream from the upper watershed, meaning that the flood plains farther downstream on Cypress Creek were too large. However, FEMA ignored these comments. But, a developer on Little Cypress Creek also opposed the TSARP map, based on the same issue raised by the CCFCC, but submitted revised analyses. Therefore, FEMA accepted the developer’s comment.

As a result of the pending federal litigation and local pressure on the map’s creator – the HCFCD – to correct the errors, the 100-year flood plain map for Cypress Creek is now in the process of being corrected through a FEMA process known as a Letter of Map Revision (LOMR). At this time, the federal court receives reports from FEMA that track the progress of the LOMR process that will lead to a much larger flood plain in the upper portion of Cypress Creek. In fact, the flooded area is sufficiently larger than it originally appeared to such an extent that the flood waters will now flow over the watershed divide and into Addicks Reservoir. To date, this overflow area has not been fully identified on the flood plain maps, and the overflow area which feeds into the Buffalo Bayou watershed is not included in this LOMR, yet there is little doubt that this overflow area exists.

GGP-Bridgelands, the owner of a 13,000 acre tract, was displeased with the proposed LOMR and was granted permission to intervene in the federal case. While only 1,500 acres of the GGP tract was in the Cypress Creek flood plain before the map revision, the revised map shows a significantly larger percentage as being flood-prone. Judge Rosenthal has stayed Sierra Club until the LOMR is accepted, or until April 8, 2009. In the meantime, FEMA must report to the court every two months on the status of the LOMR as it progresses through the FEMA process.

3. Housing Regulations Tied to Hurricane Surge Tides are Inconsistent

Hurricane Ike caused the issue of coastal flooding to be clearly visible. The Bolivar Peninsula is virtually wiped out. Aerial photos of the City of Gilchrist show that few structures remain, if any. Substantial damage was done to the West End of Galveston Island as well as the City of Galveston and west shoreline of Galveston Bay. But as bad as Ike was, it was not a Category 4 storm. The night before Ike hit, a storm surge as high as 25 to 30 feet was predicted for Galveston Bay, the same as the surge tide that hit the Mississippi Coast with Hurricane Katrina. Luckily, the “eye” slid to the north and Galveston Bay missed the dirty side of Ike. Our coastal damage, which was extensive, could have been substantially worse.

The National Flood Insurance Program involves the regulation of development along the coast in addition to insurance. However, there seems to be a disconnect between the 100-year “flood” elevations found on the FEMA flood insurance maps and the range of surge tides that are predicted along the Texas coast in association with major hurricanes. In fact, there is a major discrepancy.

FEMA flood insurance maps provide elevations for setting the first floor slab of homes along the Gulf Coast. On the West end of Galveston Island, these elevations are approximately 16 to 17 feet, and are of a similar height along the west side of Galveston Bay. However, about two hundred feet inland, the higher surge tide elevations no longer apply. New construction in the Clear Lake City area, for example, as well as in the areas of Kemah, Seabrook and Shoreacres, all somewhat removed from the shoreline, are required to meet slab elevations of about 12 feet above sea level. Surge tide models from the University of Texas show the entire Houston area east of Interstate 45 to be subject to inundation from a 22- foot surge tide that would likely accompany a Category 4 storm, with wind-driven waves atop that surge tide. Unbelievably, we as a community are allowing new construction with slabs at such low elevations. No doubt that we are asking for a new disaster unless we change these maps and change them soon. We are doing no one a favor by keeping these flood elevations so low.

Homes are not the only developments regulated by coastal flood elevations. Virtually all hazardous waste storage, industrial waste disposal, solid waste disposal, radioactive waste storage and wastewater treatment plants as well as oil storage tanks are subject to siting regulations by the Texas Commission on Environmental Quality and the U.S. Environmental Protection Agency. These regulations routinely require that these types of facilities be protected from a 100-year flood. In the case of the Houston Ship Channel, this flood level is about ten feet lower than the storm surge projected for the Ship Channel in association with Hurricane Ike. We are fortunate that this disaster did not occur. However, we are now warned of the inadequacy of our current level of protection from flooding along the Ship Channel and other coastal areas.

If a Category 4 storm occurs and, as a result, hazardous waste becomes spread over neighborhoods adjacent to the storage area, would there be any liability for such an event? Would the waste companies owe any liability to their neighbors? Is it sufficient to respond that the company built its facility to government requirements even if it were clearly reasonable on the basis of Katrina and Rita and Ike to expect a much higher coastal surge tide than was shown on the maps? The courts will be filled when such events occur and these questions will be answered.

Conclusion

It is unfortunate that government regulations are inadequate to protect our property from becoming flood-prone due to upstream development, and to protect us from hazardous waste being flushed out of storage areas. More independent oversight and accountability must occur. Moreover, it is virtually impossible for government entities such as the Harris County Flood Control District to provide adequate flood prevention and protection to the community as long as it is governed by a Commissioner’s Court that is responsible to its constituents (contributors) for an ever increasing tax base. Additionally, as long as it is easier for developers to claim a regulatory taking due to stronger regulations than for homeowners to claim property damages due to a lack thereof, the scales of justice will remain unbalanced. But times, they are a-changing. In the last few seasons, costs continue to increase and economic losses continue to soar. We have seen with Ike that the Feds are not as loose with the cash flow as they were after past storms. When communities fail to be subsidized for reckless planning, they will start to pay attention. And, just maybe, a jury will render judgment.

James B. Blackburn, Jr. is a partner at Blackburn Carter, P.C., a firm devoted to environmental law and planning, and a professor of the practice in the Department of Civil and Environmental Engineering at Rice University. A graduate of the University of Texas School of Law with an M.S. in environmental science from Rice University, he is the co-founder of Houston Wilderness, the Matagorda Bay Foundation and the Galveston Bay Foundation.

Lawrence G. Dunbar is a senior partner at Dunbar Harder PLLC and a registered professional engineer specializing in hydrology. He has a B.S. dgree in civil engineering from the University of Notre Dame, an M.S. in environmental engineering from the Illinois Institute of Technology, and a law degree from the University of Houston Law Center.

Endnotes

1. See Kraft v. Langford, 565 S.W.2d 223 (Tex. 1978). 2.Tex. Water Code §§ 16.236 & 16.237. 3. In this regard, no bayou is more infamous than Brays Bayou in southern Harris County, which became the “poster child” for flooding caused by urban development upstream. 4.Kerr v. Harris County, No. 837,329 (Co. Ct. at Law No.1, Harris County, Tex., August 27, 2008) (Set for Trial Feb. 9, 2009). 5.Kerr v. Harris County, No. 01-02-00158-CV, 2005 WL 568403 (Tex. App. -Houston [1st Dist.], March 10, 2005). 6.Sierra Club v. FEMA, No. 4:07-cv-00608, (S.D. TX, Aug. 11, 2008).

Texas, Our Texas

Texas, Our Texas! all hail the mighty State!

Jim Blackburn, environmental attorney from Houston and one of the original guiding lights for the conservation of our bays and coasts, writes an annual coastal update that he distributes in January. I have placed his latest on the One Galveston file server, and it can be accessed here.

John Anderson has written a thoughtful response to the questions raised by Jim, and he has graciously allowed for me to publish his letter, as follows.

Jim

Thanks for taking the time to do the Coastal Update. I always enjoy reading it.

With regard to your question concerning the State’s stewardship of the coast, I agree with Bob Moore, the answer is NO. As a long time researcher in Texas coastal geology, let me focus my remarks on a major problem with scientific research. I apologize if it reads like I have an ax to grind, it is not intended to come of that way, but rather to convey a problem in the way we do coastal science in Texas.

If you take a look at published results (peer-reviewed is the only true gauge of high level research in my opinion as it has passed the scrutiny of experts in the field) from scientific research along the Texas coast you will see that Texas lags behind many states, such as Louisiana, Florida, North Carolina and New Jersey, even though we have a lot of coastal real estate and one of the more interesting coasts in the world for investigation of coastal processes. Ours is also the second most vulnerable coast (Louisiana being first) to sea-level rise, subsidence and limited sediment supply. Why then is Texas not a leader in coastal research?

For decades the State of Texas has provided a minimal amount of funding for coastal research. We have done a good job of monitoring coastal erosion and that is important, but it is not science. We know our coast is eroding rapidly, both on the Gulf and Bay side of barriers, but we do not know why, how erosion will vary as the rate of sea-level rise increases, or how we might best minimize these impacts. There is an emerging scientific consensus that tropical storm frequency and magnitude will increase this century but how will that impact our coast? To what extent have humans altered sediment supply and distribution along the coast and in estuaries? These are only a few questions that require immediate attention if we are going to sustain our coast for future generations.

The State spends millions of dollars a year dumping truck loads of sand on beaches, only to have it wash away with the tides. This is unthinkable and reflects the total lack of understanding of the problem by Mr. Patterson and his people. The money spent on such projects would fund a lot of good research on wetlands ecology, sediment transport and other fields. You may not know that the only source of state funding for academic research requires that the grantee be at a State-supported university. This prevents researchers from other states and private universities (yes Rice included) from applying for state grants to work in Texas. The reality is there are relatively few scientists at state universities doing coastal research. The response from Mr. Patterson might be that various state agencies do our research, but if you count the publications over the past ten years from these agencies the number is deplorable given the amount of money that is spent, and most of that work has been done by a handful of good scientists who have somehow managed to prevail under difficult conditions. I have trained some outstanding young coastal geologists in my career who have gone on to universities in other states. They continue to be very active in the field, but not in Texas. So, we train the talent we need, they just can’t work in Texas. The final result is that our knowledge of coastal processes, such as tidal inlet dynamics, wetlands growth and development and sand transport within the coastal zone is limited, certainly no where near what it should be for us to answer questions about how our coast will respond to global change.

One might ask, so why not go to NSF or some other funding agency? This is what we have done in the past, but the reality is that NSF views coastal research at the regional scale as something the states should be supporting and most states do fund coastal research. I am not aware of another state that so discourages coastal scientists from from doing research in their state.

Jerry Patterson has his Coastal Coordinating Board, but that body is seriously deficient in scientific expertise. Most are political appointees, which is consistent with Mr. Patterson’s way of doing business. Meanwhile, our coast continues to change at a rate that astounds us all and we really don’t understand what is happening or what to do about it. We need more scientific understanding of our coast if we are going to protect it in the future, but I am not sure how the needed research is going to be done unless we encourage scientists to cross our borders.

John

John Anderson

Maurice Ewing Professor of Oceanography Department of Earth Sciences

Rice University Houston, Texas 77251-1892

Within my field, sustainable tourism and recreation, I am afraid the the same is true. The best work is being done outside of Texas, with rare exceptions such as Corpus Christi. Those who choose this profession, by necessity, are forced to work elsewhere (me being a perfect example). Given the situation that Galveston faces, one would expect sustainable recreation, tourism, and community development to be helping shape the future of our resurrected community. In my opinion, this is simply not the case. Allowed to their own devices, community interests will focus on patching Galveston back together in the same pathetically vulnerable condition that existed pre-Ike. I can only pray that there are enough of us on the island that can help direct Galveston’s future toward sustainability. The Long-Term Community Recovery Committee, under the leadership of Betty Massey, is, I hope, a step in the right direction. But what I still fail to see is the passionate, daring leadership willing to take hold of this situation and shake it into shape.

Time is passing, and we are still worried about who is winding the clock.

Ted Eubanks

Galveston’s Strategic Retreat by Ted Eubanks

The brouhaha over the buyout of beach front dwellings has flamed into an inferno. Many demand that the Hazard Mitigation Grant Program money be spent in less affluent neighborhoods in the central city, repairing homes that may well attract residents back to the city. Heber Taylor, editor of the GCDN, has argued this case repeatedly and effectively. As recently as today Heber is bemoaning the fact that West Enders are getting a sweet deal on their homes.

There is merit to both arguments, I believe. I live in the central city, and I would love to see hazard mitigation money be used to redevelop the contracting neighborhoods that surround me. But I also see how a strategic buyout on the west end offers an opportunity to address our flood risks in a unique fashion. To be honest, One Galveston should address both of these issues, no matter income levels or geographical location,.

For the moment let me focus on the west end. In recent weeks there has been a push for Galveston to consider armoring the entire length of the west end of the island. This “Ike Dike” would connect with a series of retractable or collapsible flood gates at Bolivar Roads, San Luis Pass, and across the GIWW. Even though the cost of such a massive project would be many billions of dollars, there has been little critical debate concerning its merits (like, would it work?). Galveston’s mayor and the county judge have already sped ahead with lobbying for this approach without critical analysis (or thought). If we are going to spend billions on such a massive structure, shouldn’t we at least know that it is not a Maginot Line?

During my past week’s recovery, I have had the chance to spend several days reviewing the literature (the only side benefit of being stuck in a hospital with a laptop). A review of the science, I found, should give us pause. Hardened or armored coasts are among the most significant causes of the loss (not gain) of beaches. In fact, Galveston’s seawall is often identified as the classic example (the beach having disappeared by 1916). Any “Ike Dike” would require continuous beach replenishment, a cost for which a source has yet to be identified (perhaps to be funded by beach front property owners?) The debate over who should pay for beach renourishment has been a point of contention around the country for decades, with many citizens objecting to being taxed to fund sand that benefits only a few.

There is an alternative to armoring the coast – a manageable or strategic retreat. In this scenario development is removed from the beach and the natural dune system is allowed to restore. In the case of west Galveston Island, the funds available for buyouts would be used to remove all beach front dwellings. Beach renourishment would still be necessary to stabilize the shore slope (the Bruun Rule), but a broad beach with an extensive dune structure would provide a buffer against all but the most severe storms. Since dune building is generally an aeolian (wind driven) process, I suspect that it would also be necessary to restrict vehicular traffic along the beaches to avoid compaction.

The same strategy of managed retreat would be necessary along the bay shore as well. Housing development should retreat to the upland properties that form the ridge of the island. The coastal wetlands should then be restored, and near shore boat traffic restricted, decreasing turbidity and allowing the once-prevalent sea grass beds to regenerate. Beach replenishment along the bay could come in the form of beneficial use of spoil from the dredging of the GIWW to extend the bay shore outward. In other words, a combination of beach replenishment and bay shore restoration with spoil would serve to widen the island and protect development in the interior.

The ultimate goal, of course, is to restore the natural buffers that once protected this island. With elevated housing limited to the interior, development can continue with limited risk. Natural beaches and wetlands will have been restored, offering residents recreational and aesthetic benefits that far exceed those available today. Significant efforts to rebuild a broad dune structure may well function in tandem with the planned flood gates at the ends of the island. In other words, Galveston may well be able to develop a cutting edge flood protection system where a majority of the structure is a restored natural system of protective dunes and wetlands.

No one is lobbying for a massive taking of property. Such a program could be accomplished by willing sellers selling to willing buyers (the government). This program would also require that the city planning department develop a progressive Comprehensive Development Plan, backed by council passing forceful rules and restrictions to insure the implementation of the plan. Of critical importance would be for rules that would disallow any new development in these buffer areas.

Today Secretary of State Hillary Clinton stated that “the time for action and realism is now” when facing the challenges of global warming. The same is true for Galveston and sea-level rise. We simply can no longer afford to blithely stumble forward, pretending that the forces of global climate change will somehow overlook our small sliver of sand.

In conclusion, the following is a summary from a study by Western Carolina University that speaks volumes to these very issues.


To reverse our losses, we must learn how to retreat from the shoreline. Where development already confronts the ocean, we must adopt corrective measures that are sure and fair. Where beaches are relatively undeveloped, we must apply preventive measures. A commitment to retreat as a guide to public policy and private investment would achieve the following goals:

  1. Reduce the loss of property and lives by replacing present high risk development with stable, safe development in suitable locations away from the open beaches.
  2. Meet increasing demand for public beaches by improving public access to natural beaches.
  3. Develop a more stable economic future for coastal communities.
  4. Eliminate unessential government spending and move coastal investment closer to a marketplace mechanism where economic decisions include realistic risk and cost without the benefit of direct or indirect government subsidies.
  5. Facilitate removal of many of the defensive structures and developments that now magnify the effects of erosion and the costs of disasters.

Stopping Erosion by Dr. John Anderson

Yesterday, Saturday January 24th, my wife Doris and I attended the town hall meeting at Sea Isle and wandered around the various booths reading the comments posted for each group. At the Environment Booth I was struck by one comment in particular that read “Stop Erosion”, which provoked me to sit down and write up this summary of the problem. Stopping beach erosion is about as complicated as stopping volcanoes from erupting and earthquakes from quaking and the sooner we accept this reality the sooner we will get on with the business of sustainable development in Galveston. I welcome questions and comments and am happy to provide scientific documentation of the statements I have made in this summary.

  1. For those who would question the importance of sea-level rise in controlling coastal retreat (erosion), consider that in the past 17,000 years, since the last major glaciation, sea-level has risen approximately 100 meters causing the shoreline to retreat approximately 80 miles from it previous location at the edge of the continental shelf to its current location.


  2. The current rate of shoreline retreat, which averages 3 feet/year along the west end of the island but in places is as much as 10 feet/year, is slow compared to times in the past when sea level was rising at a more rapid rate, at times as much as 50 feet/yr.
  3. The rate of rise in any given location is combination of eustasy (global sea level rise) and subsidence. This is called relative sea-level rise. Eustasy is fairly constant across the northern Gulf of Mexico but subsidence is highly variable. In western Louisiana the rate of subsidence is in places as much as 30 times faster than the rate of eustatic rise. Our neighbors to the east are already contending with problems that we will face by the end of this century. The rate of subsidence in Texas is significantly lower but locally is still a major contributor to shoreline change. Unfortunately, we have relatively few locations where elevation changes are being monitored and those are not all in the most ideal locations. There are ways to acquire long-term subsidence measurements but little work has been done in the field. Remember, we spend all our money in Texas dumping sand on the beach and pitifully little goes to address the real issues of why the coast is changing. If we don’t know why, we can’t begin address the problem.
  4. Sediment supply is as important as sea-level rise in controlling coastal change. If sediment is added to the coast fast enough to keep up with the rate of sea-level rise the shoreline will remain stable and even grow. This is how Galveston Island formed at a time when sea level was rising and why beaches adjacent to the north and south jetties have grown since the jetties were constructed. Sediment supply to the upper Texas coast is minimal. So, even a slow rise in sea level results in shoreline retreat. We still do not have an accurate sediment budget for the upper Texas coast. The recent study by the Corps of Engineers was a poor attempt to quantify the sediment budget and until the budget is improved it will not be possible to predict the response of the Gulf and Bay shorelines to accelerated sea-level rise. I have a PhD student, Davin Wallace, who is currently working on a more accurate sediment budget for the Texas coast.
  5. Many of the current maps that show coastal inundation through time are highly inaccurate because they simply flood the landscape with different scenarios for sea level rise. They do not account for subsidence or sediment supply. For the most part, they are best-case scenarios.
  6. The current Galveston Island Geohazard Map is a more accurate approach to predicting coastal change because it relies on historical rates of shoreline change to predict future change. However, it assumes a constant rate of sea level rise and does not take into account changes in sediment supply through time. Neither does it account for the impact of hurricanes. So, it is a best-case scenario and should be immediately adopted by the city until we have a better handle on subsidence and the sediment budget.
  7. Eustasy is controlled by the temperature of the oceans (remember water expands when heated) and the contribution from glaciers and ice sheets. There is no question but that the oceans are getting warmer as the atmosphere warms, and this is the main contributor to the current acceleration in sea-level rise. In addition, 80% of the glaciers on Earth are melting. The net result is that the rate of sea-level rise has nearly doubled (from an average of 1.8 mm/yr to nearly 3.0 mm/yr) this century. The contribution of ice sheets to sea-level rise is the greatest uncertainty when it comes to predicting future rise, but it is by far the most important in terms of magnitude. If the Antarctic Ice Sheet were to melt global sea level would rise 60 meters (~200 feet). While this is not going to happen in the next few tens of millions of years, the most current scientific evidence suggests that the West Antarctic and Greenland ice sheets are going to contribute to sea-level rise this century. At the most recent meeting of the American Geophysical Union in San Francisco one of the keynote speakers at the meeting (Dr. Eric Rignot) summarized the current scientific information on ice sheet mass balance and concluded that global sea-level rise will likely reach 5 mm/yr by the end of this century. Dr. Rignot is one of the best, most respected scientists in the field and I see no scientific justification to doubt his predictions.
  8. Let’s put Dr. Rignot’s sea-level prediction into perspective. If we want to view the world of coastal change at a time when sea level was last rising at a rate of 5 mm/yr we have to turn back our geological clocks 7,000 years. I have spent the past three decades studying the evolution of the Texas coast before and after 7,000 years. Take it from me, this was a time when our coast, including estuaries, was changing at a rate most people cannot (don’t want to) imagine. This is not science fiction, this scientific consensus based on the peer-reviewed literature. This is why we have to fight to educate people about the seriousness of the situation. We can no longer tolerate ignorance, indifference and greed on the part of those who control the destiny of our coast. We owe it to our children and grandchildren to fight for a more sustainable coast.

For additional reading consult Dr. Eric Rignot’s research.


John Anderson

Maurice Ewing Professor of Oceanography

Department of Earth Sciences

Rice University

Houston, Texas 77251-1892

Recovery Galveston – A Warning

The new Recovery Galveston website is now functioning. This is a joint effort of Lee Roane’s Galveston.com and Dolph Tillotson’s Galveston County Daily News. Potentially this is an excellent resource for the LTCRC, yet I am concerned about the signficant gaps in the information required in order for the LTCRC (and the community) to make informed decisions about our future. I realize that this is early in the process, but given the tight schedule there is little time to waste.

Let me give two examples. Two of the reports posted on the website are as much pitch pieces as information resources. The tourism analysis, by AngelouEconomics (a firm that apparently specializes in helping communities attract high-tech industries), argues in favor of beach renourishment, continued support of events such as the Lone Star Rally, and the need for more state funds to support the traditional tourism industry (in other words, the Parks Board agenda). Interestingly, the report admits that ecotourism represents 7.9% of our visitors (double those that come for conventions and cultural activities), and that the revenues from ecotourism (which the firm seems to have a poor grasp of) amounts to 7.5% of direct spending (triple that from cultural events). However, there is not a single recommendation or mention of existing nature tourism venues (such as the need to quickly restore GISP) or the organizations such as GINTC that are already working in this field. Featherfest is nowhere mentioned in the report (although Dickens, Lonestar Rally, etc. are dealt with in detail). In truth, little that they have assessed or addressed remotely reflects a sustainable tourism sensitivity.

The second report, Texas Rebounds, is a report from the Governor’s office that details the damage to various aspects of the Galveston economy and society. Interestingly, the report says little about environmental impacts other than those on the commercial fishery and forestry.

The LTCRC needs to have input from a wide variety of information sources, not only those filtered by city staff. Therefore I am requesting that there be a link to One Galveston so that the the committee can take advantage of the information provided here (such as the links to the various sources of information about sea-level rise).

The new LTCRC website is now available for the public to review. My advice is to keep a very close eye on what is being posted there. Everyone is contributing with the best of intentions, but I also believe that it is better safe than sorry.

Ted Eubanks