# Amicus Curiae Brief — Palazzolo v. Rhode Island

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## Record

- **Collection:** Supreme Court brief
- **Document type:** Amicus Curiae Brief
- **Published:** January 1, 2001
- **Citation:** 533 U.S. 606

## Text

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TAN 2 2 ad | i Fu,

No. 99-2047 :
j__ WAN 3
In The |
Supreme Court of the United States
+

ANTHONY PALAZZOLO,

Petitioner,

RHODE ISLAND ex rel PAUL J. TAVARES,
GENERAL TREASURER, and COASTAL
RESOURCES MANAGEMENT COUNCIL,

Respondents.

———e o —EEEE——EE

On Writ Of Certiorari To The
Supreme Court Of Rhode Island

¢

BRIEF OF DR. JOHN M. TEAL, DR. FRANK GOLET,
DR. JON C. BOOTHROYD, DR. R. SCOTT WARREN,
DR. SCOTT NIXON, DR. JOY ZEDLER
AND DR. ORRIN PILKEY
IN SUPPORT OF RESPONDENT

+
Tim EICHENBERG, Patrick A. PARENTEAU*
Program Counsel VeRMONT Law ScHoot
CENTER FOR Marini South Royalton, VT 05068
CONSERVATION (802) 763-8303
580 Market Street, oe >
Suite 550 Counsel of Record

San Francisco, CA 94104 Attorney for Amici Curiae

(415) 391-6204
Of Counsel

COCKLE LAW BRIEF PRINTING CO. (800) 225-694
OR CALL COLLECT (402) 342-2831

TABLE OF CONTENTS

Page

PUREE GIE WICC UEETE ceccccccccccsccccescees 1

SUMMARY OF ARGUMENT..................0005: 1

ET cc. Cah C Reese ben eeeuaseeesaeshewenes 2
A. The Functions and Values of the Salt Marsh Eco-

_ _ PPPPPEVTUTITIOTITITT TET TET TELE 2

B. The Ecological Effects of Salt Marsh Destruction.. 10
C. Water Quality and Public Health Impacts of

Coastal Development ...............cceeeeeeees 13
D. The Hazards of Coastal Development.......... 16
SED ac bb Cth cU ss dsvetdecicecoecesceceees 22

RPI A cc ccccccsecccvccccesenescesesevess App. 1

ii
TABLE OF AUTHORITIES

Cases

Lucas v. South Carolina Coastal Commission, 505 U.S.

BGG (UGUEP. oc cccccccecesse0se05 Nunn

United States v. Riverside Bayview Homes, Inc., 474

US. 328 (300)... ccnccccueueecheuue ene

STATUTES
Federal

16 US.C. 1908......00:00ss005cnenneneeeeeeee
16 UGC. OBB. ...00000000000sennneeneeeeeee
26 U.S.C. 160R(1) .....0+0000000050nnneneeneeen
16 U.S.C. 26BBER) ...60050000500000nnueeeenee
16 US.C. 1600D. ....<:..0s<0005s5nenneeeeeeeea
Tova
16 U.S.C. 1455b(g)(5) ... 2.0... cceeceeeeuueeeeeees
RS Coe

Rhode Island

P.L. 1965 ch. 140, § 1, G.L. 1956 §§ 2-1 - 2-17.....
P.L. 1971 ch. 279 § 1, G.L. 1956 ch. 23 of title 46..
Rev. Pub. Laws, pp. 492-97 (1798)............0005.
G.L. 1938 ch. 634, § 2... scccccsesceunenneeneee

OTHER AUTHORITIES

Brown, C., Hurricanes and Shoreline Changes in
Rhode Island, Hurricane in Southern New Eng-

land (Gordon, B., ed.) (1976). ...........ccecuees

iii
TABLE OF AUTHORITIES - Continued

Chabreck, R.H., Coastal Marshes: Ecology and
Wildlife Management (1988) .................-.

Coastal Resources Management Council, Rhode
Island’s Salt Pond Region: A Special Area Man-
agement Plan (1984)......... 2... 6. e eee ee eens.

Coastal Resources Management Council, Rhode
Island’s Salt Pond Region: A Special Manage-
ment Plan (Maushaug *o Point Judith Ponds)
EEE EEE EEE TOTTTTLITILILITT Te

Dahl, T.E., Wetlands: Status and Trends in the
Coterminous United States, mid 1970's to mid
1980's, U.S. Department of the Interior (1991)..

Desbonnet, A.P., et al., Vegetated Buffers in the
Coastal Zone: A Summary Review and Bibli-
ography, University of Rhode Island Coastal
Resources Center and Rhode Island Sea Grant
Ee ecebcebehedddeoedsocceesccecocecces

Frayer, W.E., et al., Status and Trends of Wetlands
and Deepwater Habitats in the Coterminous
United States, 1950’s to 1970’s, U.S. Department

se tic ecosedueeeeooce ce

Friedman, R.M. and DeWitt, C.B., Wetlands as Car-
bon and Nutrient Reservoirs: A Spatial, Historical,
Social Perspective, Wetland Functions and
Values: The State of Our Understanding, Pro-
ceedings of the National Symposium on Wet-
lands, November 7-10, American Water

Resources Assn. (1979) ............ccceceeeeees

Greeson, P.B, et al., Wetland Functions and Values:
The State of Our Understanding, Proceedings of
the National S ium on Wetlands, Novem-
ber 7-10, American Water Resources Assn.

— FESEEPPPPPPPTTTTTTTTTLTTTTTT ETT T Te

iv

TABLE OF AUTHORITIES - Continued

eUE Cvénnésccducéccnceseseceseséecusenetésconcees

The J. John Heinz III Center for Science, Eco-
nomics and the Environment, The Hidden Costs
of Coastal Hazards (2000) ........................

Hoffman, J.S., Keyes, D. and Titus, J.G., Projecting
Future Sea Level Rise, U.S. Environmental Pro-
See Gy Gb 060 erkéceduensecécacceccotss

IPCC Working Group I, The Science of Climate
Change (Second Assessment Report) (1995) .......

IPCC, Report to the Sixth Conference of the Par-
ties of the United Nations Framework Conven-
tion on Climate Change (Nov. 20, 2000)...........

IPCC, Special Report on Land Use, Land Use
Changes, and Forestry (1998) .....................

Kana, T.W., et al., The Physical Impact of Sea Level
Rise in the Area of Charleston, South Carolina, in
Barth and Titus, Greenhouse Effect and Sea
Level Rise: A Challenge for This Generation
SoA 0cus cocesccundusedueencesentenseudessosness

Knudson, P.L., et al., Wave Dampening in Spartina
Alterniflora Marshes, Wetlands (Journal of the Soci-
ety of Wetland Scientists) 2 (1982)..................

Lee, G.F., et al., Effects of Marshes on Water Quality,
in Coupling of Land and Water Systems (A.D.
ts CI a

Lee, Virginia, An Elusive Compromise: Rhode
Island Coastal Ponds and Their People (1980).....

Lee, Virginia and Olson, Stephen, Eutrophication
and Management Initiatives for the Control of
Nutrient Inputs to Rhode Island Coastal Lagoons,
Eotuaries Vol. § No. 2B (1996)... ccccccccccccecs

v

TABLE OF AUTHORITIES - Continued

Page

Myshrall, D.H.A., et al., Salt Marsh Restoration
Monitoring at the Galilee Bird Sanctuary, Nar-
ragansett, R.I. (2000) ........ 0... 0c cece cece eee eeeees

Niering, W.A., Endangered, Threatened, and Rare
Wetland Plants and Animals of the Continental
United States, National Wetlands Newsletter (May-

Jeune 1987)... 0.0... cc eeeccccccccccccccccessevccvees

Nixon, Scott W., Coastal Marine Eutrophication: A
Definition, Social Causes, and Future Concerns,
Ophelia 41 (1995) .........:ec cece eee ee eee eeeeeeees

Nixon, S.B., et al., Nutrient Inputs to Rhode Island
Coastal Lagoons and Salt Ponds: Final Report to
Rhode Island Statewide Planning (1982).............

Nixon and Pilson, Nitrogen in Estuarine and Coastal
Marine Ecosystems, Nitrogen in the Marine Envi-
gomment (1963) ....... cc cee cc ccccecccecceecceceees

Oceans and Coastal Resources: A Briefing Book, 23
Congressional Research Service Rep. 97-
SOGHINR (1997). ......cccccccccccccccccccsccccece 4,

Office of Technology Assessment, Wetlands: Their
Use and Regulation (1984) ...........-02eeeeeeeeeee

heim, T., Wetland Losses Have Continued but
Have Slowed, National Wetlands Newsletter (Nov.-

Peters, R., and Lovejoy, T., Global Warming and
Biological Diversity (1993) .........--+++e+eeeeeees

The Providence Journal, Sept. 8, 1954........----+++++

vi

TABLE OF AUTHORITIES - Continued

Revkin, A., Scientists Now Acknowledge Role of
Humans in Climate Change, The New York Times

SY GS MEI ane6dcccscerccnconceueesétce

State of Rhode Island Coastal Resource Management

Pt Didi on padéseneddekesaenbedddbandiabnne

Teal, J.M., Salt Marshes: They Offer Diversity of Hab-

ina I i

Teal, John and Mildred, Life and Death of the Salt

ct ccksbeidendelenetchcudecducuseuce

Tiner, R.W., Wetlands of Rhode Island, U.S. Fish and
Wildlife Service, National Wetlands Inventory

EN 46 0c cncensensednccceséoseéeceaccouceesses

Titus, J.G. and Narayanan, Vijay, The Probability of
Sea Level Rise, U.S. Environmental Protection

EY Gn 6006000 cédedcecceacecncuseesees

Titus, J.G., et al., Greenhouse Effect and Sea Level
Rise: The Cost of Holding Back the Sea, Coastal

CE EE ci idilc sencuudneneascenece

U.S. Army Corps of Engineers, Hurricane Survey
Interim Report, Narragansett Pier, Rhode Island,

Se An budeadcncduceddedecdntsanssecteces:

U.S. Environmental Protection Agency, National
Water Quality Inventory: 1994 Report to Congress

SP +6 bRedncencdendecddenesuseeunedeeucecdeses

U.S. Fish and Wildlife Service, 1996 National Sur-
vey of Fishing, Hunting, and Wildlife-Associated

I i ie a

Page

STATEMENT OF INTEREST

Pursuant to Supreme Court Rule 37, we file this brief
with the consent of the parties as amici curiae in support
of Respondent, the State of Rhode Island.'

Amici are distinguished scientists with special exper-
tise in America’s coastal and estuarine ecosystems. Scien-
tists authoring this brief include members of the National
Academy of Sciences, and leading authors on estuaries,
salt marshes, salt ponds, water quality, coastal barrier
systems, and coastal hazards. Amici include scientists
who have served on scientific panels advising govern-
ment bodies on management of coastal ecosystems. Sev-
eral have direct experience with the Rhode Island Coastal
Resources Management Program and are quite familiar
with the physical setting of this case and with the scien-
tific and technical issues presented. Appendix A contains
a brief biography of each scientist.

o

SUMMARY OF ARGUMENT

This Court has recognized that “coastal property may
present such unique concerns for a fragile land system”
that a state may be justified in restricting inappropriate
development in the most sensitive and hazardous areas
without running afoul of the Fifth Amendment. Lucas v.
South Carolina Coastal Commission, 505 U.S. 1003, 1035
(1992) (Justice Kennedy, concurring). As the majority in

1 This brief was not authored in whole or in part by counsel
for a party. The Beldon Fund contributed $2500 towards the cost
of preparing and printing this brief.

Lucas pointed out, it is important, when evaluating regu-
latory takings claims, to carefully consider the “degree of
harm to public lands and resources, or adjacent private
properties, posed by the claimant's proposed activities,”
as well as “their suitability to the location in question.”
Id. at 1031. The following information is intended to
provide the Court with a clearer picture of the geographi-
cal, ecological, and hazardous conditions that make the
salt marsh ecosystem precisely the kind of place that is
not suitable for the intensive and poorly planned devel-
opment Petitioner wishes to put there.

®

ARGUMENT

A. The Functions and Values of the Salt Marsh
Ecosystem.

Viewed from above, the coastline of Rhode Island,
like much of the eastern seaboard, reveals a striking
mosaic of interconnected geological features and biolog-
ical systems. Barrier beaches and coastal dunes front the
ocean, absorbing the sometimes violent energy of wind
and waves in their shifting sands. Behind the dunes lie
the great salt ponds, brimming with life, running parallel
to the coast like a string of pearls. Arrayed along the back
of these barrier ponds and along the tributaries and
embayments are the salt marshes, blanketed in tidally-
influenced grasses (Spartina alterniflora), the principal
food factory for this rich estuarine system. Woven into

this natural fabric are uplands and dunes, adding still
more diversity.”

This is a remarkable landscape: dynamic, diverse,
productive, beautiful, dangerous. Here the work of
nature is spectacularly displayed, bestowing rich gifts
upon the human inhabitants. One of the keystones of this
coastal environment, and_the focus of the controversy
here, is the salt marsh ecosystem. Salt marshes are
among the most biologically productive ecosystems on
earth, rivaling the richest agricultural land in terms of
organic output.* Salt marshes are the “primary pro-
ducers” that fuel the complex web of life within the
coastal estuarine system, while providing a critical nurs-
ery and “refugia” for fish and shellfish of enormous
economic and cultural importance. But these systems do
much more than simply produce biomass. A partial
inventory of the functions and values of this ecological
system would include the following.

Fish and Wildlife Habitat

As this Court has previously recognized, wetlands
“serve significant natural biological functions including
food chain production, general habitat, and nesting,
spawning, rearing, and resting sites for aquatic species.”

2 See generally, John and Mildred Teal, Life and Death of the
Salt Marsh (1969); Chabreck, R.H., Coastal Marshes: Ecology
and Wildlife Management, 21-28 (1988).

3 Tiner, R.W., Wetlands of Rhode Island, U.S. Fish and Wildlife
Service, National Wetlands Inventory, 59-60 (1989) (hereafter,
Wetlands of Rhode Island).

United States v. Riverside Bayview Homes, Inc., 474 U.S. 121,
134 (1985).

Salt marshes are the crown jewels of wetlands, sup-
porting an extensive complex of terrestrial and marine
biological diversity by providing a variety of habitats and
landscapes at the edge of the sea.4 Many different life
forms — aquatic, terrestrial, marine, freshwater - come
together in this transition zone. The marsh integrates
land and sea, pulsing with life in rhythm with the tides.

Approximately 70% of the commercial fisheries in the
United States depend on estuaries and salt marshes for
nursery or spawning grounds.® In 1995, the commercial
fishery catch totaled 4.5 million metric tons and was
valued at a record $3.8 billion.* Seafood is a significant
component of the American diet, and a major sector of
the economy. In 1995, Americans consumed an average of
15 pounds of seafood per person, and spent a total of
$38.6 billion.”

Coastal wetlands are crucial for the existence of
many birds, ranging from waterfowl, wading birds, and
shorebirds to wetland-dependent songbirds. Some spend
their entire lives in wetland environments, while others

4 Teal, J.M., Salt Marshes: They Offer Diversity of Habitat, 14
Oceanus 13 (1996)

* Id. at 55. Among the more familiar wetland-dependent
fishes are menhaden, bluefish, flounder, white perch, sea trout,
mullet, croaker, striped bass, and drum.

® Oceans and Coastal Resources: A Briefing Book, 23
Congressional Research Service Rep. 97-588ENR (1997)
(Hereafter, Oceans and Coastal Resources)

7 Id. at 35.

primarily use these areas for breeding, feeding or rest-
ing.®

The survival of many rare, threatened and endan-
gered plants and animals depends upon coastal marshes.
About 50% of the animals and 28% of the plants listed as
threatened and endangered species under the Endan-
gered Species Act, 16 U.S.C. § 1331, are wetland-depen-
dent.’ According to the Rhode Island Natural Heritage
Program, approximately one-third of all the State’s rare
plants occur in salt marshes and estuarine waters.!°

Water Quality

Wetlands help maintain water quality in several
ways: (1) by removing, retaining, and transporting nutri-
ents such as nitrates and phosphates, (2) by processing
chemical and organic waste, and (3) by reducing sedi-
ment loads.'! Wetlands are particularly good water filters
because of their location between fast land and open

8 A recent survey of birds at the Galilee Bird Sanctuary in
Narragansett, R.I. revealed 76 species of waterbirds and 42
species of landbirds. Key wetland-dependent breeding birds
included Green Heron, American Black Duck, Mallard, Clapper
Rail, King Rail, Killdeer, Willet, Marsh Wren, and Saltmarsh
Sharp-tailed Sparrow. Myshrall, D.H.A. et al., Salt Marsh
Restoration Monitoring at the Galilee Bird Sanctuary, Narragansett,
R.I., 17-19 (2000)

9 Niering, W.A., Endangered, Threatened, and Rare Wetland
Plants and Animals of the Continental United States, National
Wetlands Newsletter, 16-19 (May-June 1987)

10 Id. at 55.

1! Lee, G.F. et al., Effects of Marshes on Water Quality, in
Coupling of Land and Water Systems (A.D. Hastler, ed.) (1975)

water. They can intercept runoff from land before it

reaches water and help filter-out nutrients, wastes and
sediment. !2

Perhaps the best known demonstration of the purify- |

ing capabilities of wetlands is Tinicum Marsh, a 512 acre
tidal marsh lying south of Philadelphia, Pennsylvania.
Three sewage treatment plants discharge treated waste
into the marsh. On a daily basis, the marsh removes 8
tons of biological oxygen demanding waste, 5 tons of
phosphorous, 4 tons of ammonia, and 138 pounds of

nitrate. In addition, the marsh adds 20 tons of oxygen to
the water each day.'3

| Coastal wetlands also play a valuable role in reduc-
ing turbidity of flooding waters. This is especially impor-
tant for aquatic life and for reducing siltation of ports
harbors, rivers, and reservoirs. Removal of sediment load
is also valuable because sediments often transport

adsorbed nutrients, pesticides, heavy metals, and other
toxins.

Flood and Shoreline Erosion Control

Coastal areas are particularly susceptible to floods
and storms, as discussed in greater detail below. Coastal

'2 See generally, Greeson, P. B. et al., W
| " » RB. -, Wetland Functions and
score The State of Our Understanding, Proceedings of the
ational Symposium on Wetlands, November 7-10, American

Water Re
Values) sources Assn. (1979) (Hereafter, Wetland Functions and

‘8 Wetlands of Rhode Island, supra n.3, at 58.

marshes and floodplains, because of their strategic loca-
tion between the open ocean and upland, help protect
upland areas from erosion while providing other valuable
ecosystem services. Wetland vegetation can reduce shore-
line erosion in several ways, including (1) anchoring sedi-
ments, (2) dampening wave action through friction, and
(3) reducing current velocity through friction." Coastal
marshes and barrier beaches are far more resilient to
erosion than adjacent upland areas. They tend to recover
over time as a result of sedimentation and accretion
induced by tidal flow during quiet periods. Uplands,
once eroded, have little or no potential for recovery
except through human effort. The economic benefits of
these functions are substantial. Property owners within
the coastal zone receive reciprocal benefits from main-
taining the integrity of these natural flood control and
storm buffering features of the salt marsh ecosystem.

Climate Control

Wetland soils typically are highly organic and serve
as “sinks” for carbon.'5 As these soils are drained or
otherwise disturbed, they tend to oxidize, releasing car-
bon dioxide to the atmosphere and contributing to global
warming. An overwhelming majority of scientists now

14 Knudson, P.L., et al., Wave Dampening in Spartina
Alterniflora Marshes, Wetlands (Journal of the Society of Wetland
Scientists) 2:87-104 (1982)

15 Friedman, R.M. and DeWitt, C.B., Wetlands as Carbon and
Nutrient Reservoirs: A Spatial, Historical, Social Perspective, in
Wetland Functions and Values, supra n.12, at 175-85.

believe that anthropogenic (human) sources of carbon
dioxide and other “greenhouse gases” are at least partly
responsible for the documented increases in the earth’s
temperatures and changing weather patterns around the
globe.'° The Intergovernmental Panel on Climate Change
(IPCC), a United Nations advisory group comprised of
2500 scientists, recently revised their projected warming
trends upwards with a consequent increase in negative
environmental impacts from such effects as rising sea
levels. It is now widely accepted that sequestration of
carbon in natural systems such as wetlands and forests is
a critical component of any successful strategy to deal
with the pressing problem of global warming.!”

Recreation and Aesthetics

Many recreational activities take place in or around
wetlands. Hunting and fishing contribute significantly to
the local and national economies. In 1996, 77 million U.S.

'e As the Chairman of the Intergovernmental Panel on
Climate Change recently reported to the United Nations:

[T]he overwhelming majority of scientific experts,
whilst recognizing that scientific uncertainties exist,
nonetheless believe that human-induced climate
change is already occurring and that future change is
inevitable. It is not a question of whether the Earth’s
climate will change, but rather by how much, how
fast and where.

IPCC, Report to the Sixth Conference of the Parties of the United

Nations Framework Convention on Climate Change, November
20, 2000.

17 See, IPCC, Special Report on Land Use, Land Use
Changes, and Forestry (1998)

residents participated in wildlife-related recreation activ-
ities..8 During that year 35.2 million people fished, 14
million hunted, and 62.9 million enjoyed at least one type
of wildlife-watching activity. Expenditures associated
with wildlife-related recreation totaled $101 billion in
1996.19

It is much harder to put a dollar value on the sheer
beauty of the coast, and the sense of awe and wonder it
inspires. Perhaps the image painted by naturalist-author
John Hay will suffice:

I sat on the sands and listened to the sonorous
heave and splash of low waves. The sun, like a
colossal red balloon filled with water, was sink-
ing in to the horizon. It swelled, flattened, and
disappeared with a final rapidity, leaving a
foaming, fiery band behind it. I suddenly heard
the wild trembling cry of a loon behind me, and
then saw it fly over heading north. The wind
grew cool, after a hot day when the light shone
on metallic, glittering slow waters, and sharp,
pointed beach grasses clicked together, while I
watched the darkness fall around me.?°

18 U.S. Fish and Wildlife Service, 1996 National Survey of
Fishing, Hunting, and Wildlife-Associated Recreation, 4 (1997).

19 Id.
20 John Hay, An Imagined Frontier, in The Great Beach (1964)

10

B. The Ecological Effects of Salt Marsh Destruc-
tion

According to current estimates by the U.S. Fish and
Wildlife Service (USFWS), only 5.1 million acres of
estuarine inter-tidal wetlands remain in the coterminous
United States.?! This figure represents about 5% of the
nation’s total wetlands resource.22

Between the 1950’s and 1970’s, New England saw a
major loss of coastal wetlands. For example, some 10 % of
Rhode Island’s coastal wetlands greater than 40 acres
were filled between 1955 and 1964.23 In response, coastal
states began enacting wetlands protection laws. Rhode
Island passed the nation’s first Inter-tidal Salt Marsh Act
in 1965. P.L. 1965 ch. 140, sec 1, G.L. 1956 sec 2-1 through
2-17. In 1971, Rhode Island became the first state to enact

21 Opheim, T., Wetland Losses Have Continued but Have

Slowed, National Wetlands Newsletter, 7-9 (November-December
1997)

*2 Nationwide, wetlands have been disappearing at a rapid
rate throughout most of the nation’s history. USFWS estimates
that 104 million acres remains of the 220 million that existed
when the country was first settled. Office of Technology
Assessment, Wetlands: Their Use and Regulation, 87 (1984).
Between the 1950’s and 1970's the rate of loss was over 500,000
acres per year. Frayer, W.E., et al., Status and Trends of Wetlands
and Deepwater Habitats in the Coterminous United States,
1950’s to 1970's, U.S. Department of Interior (1983). This trend
has slowed considerably thanks to stronger wetland protection
laws. Between 1985 and 1995, the net loss was 117,000. See, Dahl,
T.E., Wetlands: Status and Trends in the Coterminous United

States, mid 1970's to mid 1980’s U.S. Department of the Interior
(1991)

23 The State of Rhode Island Coastal Resource Management
Plan, 57 (1990)

11

a comprehensive Coastal Resources Management Act,
which established the Coastal Resource Management
Council (CRMC). P.L. (1971) ch.279 sec 1, G.L. (1956)
chapter 23 of title 46. In fact, Rhode Island’s concern for
protecting coastal resources dates back even further.
There were laws on the books as early as 1798 protecting
salt ponds. Rev. Pub. Laws, pp 492-97 (1798). Since 1938,
the state has prohibited the introduction of “every sub-
stance that would injuriously affect the natural and
healthy propagation, growth, or development of any fish
or shellfish in the waters of the state.” G.L. (1938) ch. 634,

Sec 1.

Today the major causes of coastal wetland losses are
urban development and encroachment of coastal water
caused by dredging projects, impoundments, and sea
level rise. The case at bar is an example of the kind of
development that would do great damage to our remain-
ing salt marshes. Petitioner seeks permission to construct
a bulkhead on the shore of Winnapaug Pond and fill
approximately 18 acres of salt marsh in order to create a
74 lot subdivision. The marsh on Petitioner's property is
part of a 160 acre salt marsh complex that extends from
Weekapaug on the east to Misquamicut on the west,
bordering the southern shore of Winnapaug Pond. J.A. 7.
The record reveals that this is “one of the more valuable
tidal salt marshes in Rhode Island.” J.A. 35. The marsh is
“extremely valuable in terms of plant species that grow
there and as habitat for birds.” J.A. 35. According to the
Field Biologist’s report:

There is overwhelming evidence that the biolog-

ical communities indigenous to this coastal wet-
land will be seriously and deleteriously effected

12

(sic) by the proposed filling and bulkheading
activity. Valuable wildlife habitat will be
destroyed outright, habitat necessary for the
survival and maintenance of the shellfish and
finfish populations will be lost, and there is a
very reasonable probability that a species of
bird and two species of plants now listed as
species of significance will be eliminated from
the area. J.A. 4.

The 18 acres of marsh on Petitioner’s property repre-
sents 12% of the salt marsh associated with Winnapaug
Pond. Given the relatively small size (approximately 2000
acres) of the pond’s watershed, this is a “highly signifi-
cant number” according to the expert testimony before
the Rhode Island Coastal Resources Management Council
(CRMC). (J.A. 35) Filling the marsh “would destroy the
natural shoreline protection, decrease sediment trapping
and accretion, decrease flood storage, and eliminate or
greatly reduce nutrient retention.” (J.A. 27)

The impacts on Winnapaug Pond are cause for
serious concern. Salt ponds are shallow, productive
estuarine embayments separated from the ocean by a
narrow barrier spit. They provide prime habitat for com-
mercial and recreational fish and shellfish, as well as
resting and feeding stops for waterfowl, wading birds,
shorebirds and other wetland-dependent birds migrating
along the Atlantic flyway. Rhode Island’s salt ponds have
been an important source of fish and shellfish for people
long before recorded histories. Archeological evidence
from the 1600’s indicates the tremendous bounty yielded
to the native peoples that first used these areas and to the

13

colonists that followed.2* These ponds have been an
important factor in the quality of life for local residents
and a prime recreational attraction for tourists in the

region.

C. Water Quality and Public Health Impacts of
Coastal Development

Rhode Island’s salt pond region, which includes Win-
napaug Pond, is especially vulnerable to water quality
problems related to the density and distribution of devel-
opment within the relatively small watersheds of the
ponds.?> Bacterial contamination and nutrient enrichment
are the primary threats to water quality. Indeed, these are
the principal water quality problems of other estuaries all
along our nation’s coasts. More square miles of estuarine
waters are polluted by nutrients and bacteria than any
other type of contaminant.?¢

Sewage disposal through septic systems is a major
documented source of nitrogen and bacteria loading for
many coastal environments.” Failing and substandard

24 Virginia Lee, An Elusive Compromise: Rhode Island
Coastal Ponds and Their People, 22 (1980)

25 Coastal Resources Management Council, Rhode Island's
Salt Pond Region: A Special Area Management Plan, 25 (1984).

26 U.S. Environmental Protection Agency, National Water
Quality Inventory: 1994 Report to Congress, 11 (1995)

27 Nixon, S.B., et al., Nutrient Inputs to Rhode Island Coastal
Lagoons and Salt Ponds: Final Report to Rhode Island Statewide
Planning (1982); Nixon and Pilson, Nitrogen in Estuarine and
Coastal Marine Ecosystems, in Nitrogen in the Marine
Environment (1983)

14

individual sewage disposal systems (ISDS) and resultant
contaminated runoff are the principal sources of bacterial
contamination to the salt ponds. In fact ISDS’ contribute
almost ten times as much as any other source of nitro-
gen. Most of the existing residential and commercial
development in the salt pond region, including the Win-
napaug Pond watershed, rely upon ISDS for disposal of
sewage. Petitioner's development would also rely on
ISDS. J.A. 8

Excess input of nutrients leads to eutrophication of
water bodies. In marine ecosystems nitrogen is the essen-
tial nutrient that stimulates plant growth. As nutrient
loading increases in salt ponds, massive growth of algae
occurs and the dissolved oxygen necessary for aquatic
life is depleted. During extreme low oxygen events,
hypoxia (less than 3 mg of oxygen per liter) or anoxia (all
the dissolved oxygen is consumed) can occur with conse-
quent fish kills, reduced biodiversity of fish and shellfish
populations, mass mortality of benthic organisms, bacte-
rial slimes, foul smelling odors, and in some cases toxic
levels of hydrogen sulfide.2® Eutrophication of estuaries
has become a major issue in Rhode Island and other
coastal states.*°

28 CRMC, Rhode Island’s Salt Pond Region: A Special
Management Plan (Maushaug to Point Judith Ponds), ch. 1, at 6
(1999) (Hereafter, Salt Pond SAMP).

2? Nixon, Scott W., Coastal Marine Eutrophication: A
Definition, Social Causes, and Future Concerns, Ophelia 41:199-219
(1995)

% Virginia Lee and Stephen Olson, Eutrophication and
Management Initiatives for the Control of Nutrient Inputs to Rhode
Island Coastal Lagoons, Estuaries Vol. 8 No. 2B, 191-202 (1995)

ee

15

Excess loading of nitrogen to groundwater also cre-
ates serious public health problems. Nitrogen in ground-
water takes the form of nitrate, a very stable anion that is
relatively unaffected in the subsurface environment. A
high level of nitrate in groundwater is a public health
problem since groundwater is the sole source of drinking
water for public water supplies and private wells
throughout the salt pond region.*! In some areas around
salt ponds, nitrate levels already exceed safe thresholds
for drinking water.*?

In inland areas, the solution to these problems might
be to build a public sewer system. However, sewer sys-
tems encourage high density development and increase
runoff contamination of adjacent water bodies. Sewers
are an appropriate solution for urbanized areas where
other alternatives are no longer available, but not for
areas such as the salt pond region where less dense
development is both feasible and desirable. Adequate
buffer zones are needed around the salt ponds, their
tributaries and wetlands to help control nitrogen contam-
ination.*9 -

31 Salt Pond SAMP, supra n.28, at Ch 3.
32 Id.

33 Desbonnet, A.P., et al., Vegetated Buffers in the Coastal
Zone: A Summary Review and Bibliography, University of
Rhode Island Coastal Resources Center and Rhode Island Sea
Grant, 61 (1994).

16

D. The Hazards of Coastal Development

People are drawn to the coast. Nearly 50% of the U.S.
population resides in coastal areas.*4 From 1960-1990, the
population in U.S. coastal areas increased from 80 to 110
million and is projected to reach 127 million by 2010.35
Significant economic activity and growth has’ occurred as
coastal residential, commercial, and recreational develop-
ment has accelerated in recent decades. For example,
approximately 50% of annual U.S. residential construc-
tion during the past two decades occurred in coastal
areas.** Much of this development has been encouraged,
whether intentionally or not, by government-funded
infrastructure developments such as highways, water and
sewer service, causeway access, and beach nourish-
ment.*” Federal programs such_as the National Flood
Insurance Program and the Federal Disaster Assistance

Program have subsidized the risk of loss from floods and
storms.**

This increasing concentration of development along
the Nation’s coasts entails a risk to life and property from
major storms. For example, hurricane Andrew, one of the
most devastating natural disasters to strike the United
States, roared across southern Florida and into the low-

34 Oceans and Coastal Resources, supra n.6, at 41.
35 Id.
36 Id.

37 The H. John Heinz III Center for Science, Economics and
on = The Hidden Costs of Coastal Hazards, 19

38 Id.

17

lying coastal areas of Louisiana in August 1992, destroy-
ing 28,000 homes, leaving 180,000 temporarily homeless,
and affecting the lives of 275,000 residents of these two
states.3? This one storm did an estimated $30 billion in
damage. Hurricane Hugo, the 1989 storm that struck the
U.S. Virgin Islands and Puerto Rico, and came ashore at
Charleston, South Carolina, caused damage estimated at
$6 billion.” On average, two hurricanes strike the U.S.
coast each year, with two intense storms (like Andrew
and Hugo) hitting every three years.

Rhode Island is particularly susceptible to hurricane
damage. Unlike many Atlantic coastal states, its ocean
shoreline runs east-west and lies exposed to the full force
of a tropical storm approaching from the south. It is
directly in the path of most hurricanes that reach New
England before the storm tracks veer east over the North
Atlantic, and it is unprotected by large islands such as
Long Island, Fisher’s Island or Martha’s Vineyard that lie
off other stretches of mainland to the north and south.*!

In the Great Atlantic Hurricane of 1938, the southern
shore of Rhode Island experienced winds and waves of
the greatest speed and height recorded anywhere in New
England.‘42 Over 300 people lost their lives. Nearly 2000
homes were destroyed. Property damage exceeded $100
million. The storm reshaped the coastline, pushing the

39 Id. at 65.
40 Id. at 63.

41 Brown, C., Hurricanes and Shoreline Changes in Rhode
Island, in Hurricane in Southern New England (Gordon, B. ed.)
14-28 (1976)

42 Id.

18

large dunes at Weekapaug back fifty feet, eroding the
cliffs at Watch Hill by thirty-five feet, and inundating the
salt ponds and wetlands. The area around Winnapaug
Poni, including the property now owned by Petitioner,
was completely flooded out.

According to the U.S. Army Corps of Engineers, 71
hurricanes have struck Rhode Island’s shore since 1635
with an average frequency of one every seven years.* Of
course hurricanes do not stick to any schedule. After the
disastrous 1938 hurricane, many of the coastal areas were
rebuilt, additional “armoring” was installed, and then
Hurricane Carol struck in 1954, killing 19 people, destroy-
ing 3800 houses, sweeping the barrier clean, and causing
another $90 million in damage.

Hurricanes are not the only threat to coastal develop-
ment. Sea levels have been steadily rising as a result of
thermal expansion of the oceans and the melting of gla-
ciers and ice sheets in response to global warming.*> Sea

#3 U.S. Army Corps of Engineers, Hurricane Survey Interim
Report, Narragansett Pier, Rhode Island, GPO (1960)

“4 The Providence Journal, p. 1 (Sept. 8, 1954).

45 Global average temperatures have increased by 1.1
degree F since 1900. During that same time period carbon
dioxide emissions have increased by 30%. The decade of the 90’s
was the hottest one on record and 1997 was the hottest year ever
recorded. Increased globai temperatures are expected to
increase the number and severity of extreme weather events
such as floods, hurricanes and tornadoes. According to the 1995
Report of the IPCC, sea levels are expected to rise by 1 meter by
2100. IPCC, Working Group I, The Science of Climate Change
(Second Assessment Report) (1995); A. Revkin, Scientists Now
Acknowledge Role of Humans in Climate Change, The New York

19

level is rising more rapidly along the U.S. coast than
worldwide. Studies by EPA and others have estimated
that along the Gulf and Atlantic coasts, a one foot rise in
sea level is likely by 2050 and could occur as early as
2025. A sea level rise of one foot would increase the size
of the 100-year floodplain in the U.S. from 19,500 square
miles to 23,000 square miles, and increase flood damages
by 36-58 percent.

Rising sea levels will continue to inundate wetlands
and lowlands, accelerate coastal erosion, exacerbate
coastal flooding, threaten coastal structures, raise water
tables, and increase the salinity of rivers, bays and aqui-
fers. For example, studies have shown that a one meter (3
foot) rise on the Atlantic coast would result in the erosion
of from 50 to 100 meters from New England to Maryland.
This would enable a 15-year storm to flood many areas
that would otherwise only be flooded by a 100-year
storm.*” Nationwide, the total cost of damages from a sea
level rise of one meter would be $270-475 billion, ignor-
ing future development.*

Times, A-1 (October 26, 2000); R. Peters and T. Lovejoy, Global
Warming and Biological Diversity, xii-xiv (1993)

4 See, Hoffman, J.S., D. Keyes, and J.G. Titus, Projecting
Future Sea Level Rise, U.S. Environmental Protection Agency
(1995); Titus, J.G. and Vijay Narayanan, The Probability of Sea
Level Rise, U.S. Environmental Protection Agency (1995).

47 Kana, T.W., et al., The Physicai Impact of Sea Level Rise in
the Area of Charleston, South Carolina in Barth and Titus,
Greenhouse Effect and Sea Level Rise: A Challenge for This
Generation (1984)

48 Titus J.G., et al., Greenhouse Effect and Sea Level Rise: The
Cost of Holding Back the Sea, Coastal Management 19:171 (1991)

20

With potential costs of this magnitude, there will be
tremendous social and political pressure to “armor-plate”
the beach with levees and bulkheads, and to expand
“beach nourishment” projects (i.e. importing replacement
sand).4? But the environmental costs of such engineering
would be enormous. Bulkheading and filling along the
inland perimeter of a marsh prevents inland migration of
wetland vegetation as sea level rises. This kind of struc-
tural approach would eliminate most of the nation’s
coastal wetlands. A more prudent approach would be to
avoid, or if necessary to restrict, intensive development
in high hazard areas such as the one involved here.

States like Rhode Island find themselves caught
between opposing forces in dealing with these problems.
On the one hand, Congress, in the Coastal Zone Manage-
ment Act of 1972 (CZMA), 16 U.S.C. § 1451, has stated a
national policy to “encourage the states to exercise effec-
tively their responsibilities in the coastal zone through
the development and implementation of management
programs to achieve wise use of the land and water
resources of the coastal zone.” 16 U.S.C. § 1452(1). Such
programs must provide for “the protection of natural
resources, including wetlands, floodplains, estuaries,
beaches, dunes, barrier islands, coral reefs and fish and
wildlife and their habitat within the coastal zone,” as well
as “minimize the loss of life and property caused by
improper development in flood-prone, storm surge, geo-
logical hazard and erosion-prone areas.” 16 U.S.C. § 1452
(2). As mentioned, Rhode Island led the way by adopting

49 Id., at 209.
50 Id.

21

a coastal zone management program one year before
enactment of the CZMA.

In 1996, Congress amended the CZMA to add a spe-
cial program to control “nonpoint” source pollution in
the coastal zone. 16 U.S.C. § 1455b. This provision directs
states to prepare and adopt “management measures” to
control the addition of pollutants from new and existing
sources — including septic systems - that reflect “the
greatest degree of pollutant reduction achievable through
the application of the best nonpoint pollution control
practices,” including siting criteria for new development.
16 U.S.C. § 1455b(g)(5). Failure to adopt such controls
results in loss of financial assistance to implement the
overall CZMA program. 16 U.S.C. § 1455b(c)(3).

Congress has further decreed that, to qualify for
insurance coverage under the National Flood Insurance
Program, states and local communities must adopt strict
floodplain management requirements including perfor-
mance standards for new construction and a prohibition
on unnecessary and incompatible developments in spe-
cial flood hazard areas as listed on the Flood Insurance
Rate Maps required by the Flood Insurance Act. 42 U.S.C.
§ 4784.

On the other hand, when states like Rhode Island,
which has been diligent and thorough in its approach to
dealing with these difficult problems, take the steps
called for under these national policies and programs,
they are sometimes met, as here, with outraged owners of
coastal property demanding the right to do the very
things that sound coastal management says they should
not do. The fact is that Petitioner’s property is not an

22

island separate and apart from the rest of the coastal
system. Land is not merely a commodity, to be bought
and sold; it is also a community of living organisms,
human and non-human, to be respected and properly
cared for. What happens on Petitioner’s land has tremen-
dous spillover effects on other landowners and on the
ecological system which supports everything that exists
in the coast.

On the Flood Rate Maps the area in which Peti-
tioner’s property is located is labeled “V Zone” which
stands for “high hazard zone.” J.A 26. There is good
reason for the label, and the State of Rhode Island had
good cause to reject Petitioner’s proposal to place still
more lives and property at risk from the next storm to
come sweeping up the coast.

¢

CONCLUSION

For the foregoing reasons, amici urge the Court to
uphold the judgment of the Supreme Court of Rhode
Island.

Respectfully submitted,

Patrick A. PARENTEAU*
VERMONT Law SCHOOL
South Royalton, VT 05068
(802) 763-8303

*Counsel of Record
Attorney for Amici Curiae

App. 1

APPENDIX A
BIOGRAPHIES OF AMICI

Dr. John M. Teal is a Scientist Emeritus at Woods Hole
Oceanographic Institution where he was Chair of Biology.
He is a recipient of the National Wetlands Award for
Science Research from the Environmental Law Institute,
U.S. Environmental Protection Agency, U.S. Fish & Wild-
life Service, and National Marine Fisheries Service, and
the 1999 Odum Award from The Estuarine Research Fed-
eration. The author of over 140 scientific publications, his
1969 book, Life and Death of a Salt Marsh, played a major
role in increasing public awareness of the importance of
wetlands. He is a past president of the Society of Wetland
Scientists, and is also a member of Ecological Society of
America, Estuarine Research Federation, Society for Eco-
logical Restoration, American Association for the Advan-
cement of Science, Ecological Engineering Society, and
Society of Limnology and Oceanography

Dr. R. Scott Warren holds the Temple Chair in the
Department of Botany at Connecticut College. He
received his Ph.D. from the University of New Hamp-
shire, and has worked in tidal wetlands for over 25 years,
where his research has focused on salt and brackish
marsh vegetation dynamics, impacts of sea-level rise,
tidal wetland restoration, and effects of Phragmites inva-
sion on angiosperm community structure, invertebrate
populations and fish. He teaches courses in tidal marsh-
estuarine ecology, and has appeared in numerous peer-
reviewed publications and scientific meeting presenta-
tions. He is currently on the editorial board of the journal
Estuaries and served in a similar capacity for the journal

App. 2

Wetlands from 1992 — 1996. He has been president of the
New England Estuarine Research Society, the Northeast
Section of the American Society of Plant Physiologists,
and a member of the Governing Board of the Estuarine
Research Federation.

Dr. Francis Golet is Professor of Wetland Ecology in the
Department of Natural Resources Science at the Univer-
sity of Rhode Island. Dr. Golet is co-author of the Classi-
fication of Wetlands and Deepwater Habitats of the United
States, a publication that was adopted as a National Stan-
dard by the Federal Geographic Data Committee of the
Office of Management and Budget in 1996. His principal
areas of research expertise include: wetland classification,
wetland wildlife habitat assessment, forested wetland
ecology, ecology and conservation biology of wetland
songbirds, wetland vegetation dynamics, and wetland
restoration. In 1988 he received the Rhode Island Coastal
Conservation Award from the Rhode Island Coastal
Resources Management Council. For the last 9 years Dr.
Golet has been Principal Investigator for one of the larg-
est salt marsh restoration projects in New England, at
Galilee, Rhode Island; in 1999 he and his research team
received a Coastal America Partnership Award for their
accomplishments in this successful project.

Dr. Jon C Boothroyd is a Professor of Geology at the
University of Rhode Island and the Rhode Island State
Geologist. He served as the National Chair of the Geolog-
ical Society of America, Northeastern Section, Associate
Editor of the Journal of Sedimentary Research, Panel mem-
ber of the Quaternary Geology and Geomorphology Divi-
sion of the Geological Society of America, and President
of the Society for Sedimeritary Geology. He is primarily a

App. 3

field geologist specializing in coastal, braided river, and
various glacial environments with 35 years of field expe-
rience in New England, South Carolina, Alaska, Iceland,
Saudi Arabia, Madagascar, Ecuador and Mexico. He
wrote the coastal hazards section of the Rhode Island
Coastal Resources Management Plan, a special area man-
agement plan for the Salt Ponds of Rhode Island, and an
atlas and habitat inventory/resource mapping for Nar-
ragansett Bay and associated coastlines.

Dr. Joy Zedler is the Aldo Leopold Professor of Restora-
tion Ecology at the University of Wisconsin-Madison
Arboretum and Botany Department, and is the Director of
Research for the UW-Madison Arboretum. Dr. Zedler’s
research interests include restoration and wetland ecol-
ogy, role of biodiversity in ecosystem function, use of
mesocosms in wetland research, invasive plants, and
adaptive management. She helps edit four peer-reviewed
journals (Ecological Applications, Wetlands Ecology and
Management, Ecological Engineering, and Ecosystems). She
is a member of Ecological Society of America, Estuarine
Research Federation, Society for Ecological Restoration,
Society of Weiland Scientists. Dr. Zedler collaborates on
research to improve the effectiveness of salt marsh resto-
ration in southern California, and recently published
Handbook for Restoring Tidal Wetlands (J. Zedler, ed. 2000.
CRC Press).

Dr. Scott Nixon is Professor of Oceanography at the
University of Rhode Island, and Director of the Rhode
Island Sea Grant program. He is a recipient of the New
England Estuarine Research Society award for outstand-
ing contributions to estuarine research, the First “Wiese

App. 4

Lecturer” in Marine Science from the University of South-
ern Alabama, and the B. H. Ketchum Award for excel-
lence in coastal research from the Woods Hole
Oceanographic Institution. He is o-editor-in-Chief of the
journal ESTUARIES, and a member of the National
Research Council’s Ocean Studies Board, and Committees
on the Coastal Ocean, the Role of Terrestrial Ecosystems
in Global Change, and the Restoration of the Greater
Everglades Ecosystem (Vice Chair). He is also a member
of the American Society of Limnology and Oceanography,
American Society of Environmental History, and the
Estuarine Research Federation, and the author of
numerous publications on the coastal ecosystem includ-
ing, A Coastal Marine Ecosystem: Simulation and Analysis
(Ecological Studies, 1978), Coastal marine eutrophication: A
definition, social causes, and future concerns, (Ophelia 1995)

Dr. Orrin Pilkey is the James B. Duke Professor emeritus
of Earth and Ocean Science, and the Director of the
Program for the Study of Developed Shorelines in the
Nicholas School of the Environment at Duke University.
Dr. Pilkey has written more than 200 publications on
shoreline processes, erosion, barrier islands and coastal
management issues including the Corps and the Shore
(Island Press), and Living by the Rules of the Sea (Duke
Press). He is a recipient for numerous awards including
the Francis Shepard medal for excellence in marine geol-
ogy, the American Association of Petroleum Geologist’s
George V. Cohee Public Service Award, the American
Ecological Institute’s Outstanding Public Communication
Award, the Federal Emergency Management Agency’s
Outstanding Public Service Award, and the Geological
Society of America’s Public Service Award. He is the

Smee s

App. 5

former president of the Society of Sedimentary Geology,
president of the North Carolina Academy of Science,
member of the council of the Geological Society of Amer-
ica, and co-editor and author of the 22-volume Journal of

Sedimentary Petrology.

---

Source: Frix Law Library, https://www.frixlaw.com/law-library/documents/brief%3Amicro_IA40385014_0384%3A20. Public record. Not legal advice.
