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Q Ilk T-\Yo PHASE II REPORT: LTOPOGRAPHICAL SURVEY AND HYDROLOGICAL ANALYSIS OF THE WALLIS SANDS AND PHILBRICK BROOK MARSHES SPECIFIC RECOMMENDATIONS FOR DRAINAGE IMPROVEMENTS Submitted to THE TOWN OF RYE, NEW HAMPSHIRE Prepared by NORMANDEAU ASSOCIATES INC. 25 Nashua Road Bedford, New Hampshire 03102 R-4119B August 1988 TABLE OF CONTENTS PAGE 1.0 INTRODUCTION . . . . . . ... . . . . . . . . . . . . . . . . 1 2.0 HYDROLOGIC SUMMARY . . . . . . . . . . . . . . . . . . . . . 2 2.1 BASIN VOLUME ESTIMATES . . . . . . . . . . . . . . . . . 2 2.2 TIDAL VOLUME EXCHANGES . . . . . . . . . . . . . . . . . 4 2.3 STORM WATER RUNOFF SUMMARY . . . . . . . . . . . . . . . 4 3.0 RECOMMENDATIONS . . . . . . . . . . . . . . . . . . . . . . . 9 3.1 OVERVIEW . . . . . . . . . . . . . . . . . . . . . . . . 9 3.2 DRAINAGE IMPROVEMENTS . . . . . . . . . . . . . . . . . 13 4.0 LITERATURE CITED . . . . . . . . . . . . . . . . . . . . . . 29 1.0 INTRODUCTION Normandeau Associates Inc. (NAI) has completed the Topographical Survey and Hydrological Analysis of the Wallis Sands and Philbrick Brook salt marshes in the town of Rye, New Hampshire. The objective of the current study is to provide the physical basis for tidal restoration in two of Rye's salt marshes located in the Wallis Sands and Philbrick Brook watersheds. The results are presented in three phases. Phase I is an evaluation of existing conditions in the two study areas, including hydrology, topography and engineering features, and general recommendations for achieving marsh restoration. Phase II recommends specific engineering and drainage improvements to achieve optimal tidal flushing and flood protection. Phase III assesses the impacts of drainage alterations on surrounding development, including properties, septic systems, structures, and roadways. This report is a presentation of Phase II results, including 1) a summary of marsh hydrologic data; and 2) specific recommendations for engineering and drainage improvements. The New Hampshire Coastal Program provided a grant for the preparation of this report, which was funded in part by the Coastal Zone Management Act of 1972, as amended, administered by the Office of Ocean and Coastal Resource Management, National Oceanic and Atmospheric Administration. 2.0 HYDROLOGIC SUMMARY Topographic and hydrologic data were integrated in Phase I to develop general recommendations for improving stormwater drainage and tidal exchange. The following section summarizes those data that were used to develop specific design recommendations for Phase II. Some of these data were included in the Phase I report, and are reiterated here for continuity. All elevations in this report refer to the National Geodetic Vertical Datum (NGVD). Included in this section are: 1) volume estimates for all basins up to 5.0 feet NGVD; and 2) volume exchange estimates for basins with restricted flow based on tidal measurements of 16 March 1988. 2.1 BASIN VOLUME ESTIMATES Volumes of marsh basins in the Wallis Sands and Philbrick Brook marshes are given in Table 1. These estimates are based on interpretation of 1" = 1000' aerial photography and field reconnais- sance. Topographic contours were determined at 5.0-foot intervals, relative to NGVD, up to an elevation of 10.0 feet (i.e., contours were established at 0.0, 5.0, and 10.0 feet). The 5.0-foot contour approximated the transition zone from salt marsh to upland throughout the study areas, and generally corresponds to the level of spring tide flooding. Thus, the basin volume up to the 5.0-foot contour is the approximate capacity of the marsh during spring high tides which occur roughly twice per month. Basin volume estimates were used to estimate volume exchanges (Section 2.2), and to estimate water budgets for tidally restricted basins. Water budgeting yielded information on baseline freshwater inflow and percent tidal exchange used in the placement and design of drainage improvements. 2 TABLE 1. VOLUME ESTIMATES FOR INDIVIDUAL BASINS OF THE WALLIS SANDS AND PHILBRICK BROOK SALT MARSHES, RYE, NEW HAMPSHIRE. APPROXIMATE BASIN VOLUMES (CUBIC FEET) BASIN SERVED BY TIDAL CREEKS MOSQUITO TOTAL BASIN DESCRIPTION CULVERT AND PONDS DITCHES MARSH UP TO 5. 01 SURFACE NGVD WALLIS SANDS MARSH 1,043,743 45,255 3,454,609 4,543,607 South of Wallis Rd. to Concord 514,622 33,375 1,922,169 2,470,166 Washin ton Rd. and Point east of Brackett Rd. Outlet (Massacre marsh) West of Brackett Rd. 5 600 - 13,360 13,960 (upper Massacre marsh) North of Wallis Rd., 4 427,757 11,090 1,180,953 1,619,800 west of Ocean Blvd. and south of Marsh kd. East of Ocean Blvd *as 3A 32,673 300 72,007 104,980 south of Wallis San & beach parking. 3B North of Marsh Rd. 2 68,091 490 33,801 102,382 southeast of Parson's Rd. North of Parsons Rd., 1 - - 232,319 232,319 east of Brackett Rd. PHILBRICK BROOK MARSH East of Ocean Blvd. Rye 1,073,635 7,230 1,671,347 2,752,212 and south of Harbor Rd. Harbor Outlet West of Ocean Blvd., 7 & 8 45,379 1,100 225,417 271,896 south of Harbor Rd. to Locke Rd. Southwest of Locke Rd. 9 9600 3100 183,358 196,058 and west of Yushak Driveway East of Yushak Driveway 10 26,100 430 95,629 122,159 and west of Ocean Blvd. East of Ocean Blvd. and 11 - - 72,963 72,963 west of Old Beach Rd. 3 Basin volumes are given in cubic feet, and may appear immense to those unaccustomed to these units. To put these figures in perspec- tive, it is helpful to consider the sizes of the areas involved. The Wallis Sands and Philbrick Brook Study areas are approximately 185 and 100 acres in area, respectively. One acre equals 43,560 square feet, hence a foot of water covering an acre (one acre-foot) is 43,560 cubic feet in volume. One hundred acre-feet thus contains 4,356,000 cub ic feet of water. By comparison, the estimated volume of water leaving Wallis Sands Marsh at Concord Point during a single ebb tide on 16 March, 1988 was 1,819,200 cubic feet. 2.2 TIDAL VOLUME EXCHANGES Water volume exchanges were measured over a spring tidal cycle on 16 March 1988 at suspected points of restriction throughout the Wallis Sands and Philbrick Brook marshes. Points of restriction were illustrated in the Phase I report using graphs of water levels measured simultaneously on both sides of suspected pipes, culverts, sluiceways, and bridges. For Phase II it was necessary to determine the relative severity of the restrictions revealed during Phase I. To accomplish this, volume exchange measurements made on 16 March 1988 were coupled with the basin volume estimates given in Table 1. Table 2 summarizes these data and provides estimates of percent volume exchanges. 2.3 STORM WATER RUNOFF SUMMARY The effectiveness of existing structures for channeling storm- water runoff was evaluated for several scenarios of tidal height and magnitude of storm event, using HEC-1 stormwater modeling software (HEC-1 1985). HEC-1 evaluates stormwater runoff by estimating the peak 4 TABLE 2. PERCENT VOLUME EXCHANGE MEASURED IN TIDALLY RESTRICTED BASINS ON 16 MARCH 1988 IN THE WALLIS SANDS AND PHILBRICK BROOK SALT MARSHES, RYE, NEW HAMPSHIRE. FOR THESE CALCULATIONS, UPSTREAM BASINS RECEIVING TIDAL INPUT DURING SURVEY ARE ADDED TO TOTAL VOLUMES OF DOWNSTREAM BASINS. PERCENT BASIN SERVED BASIN VOLUME TIDAL TIDAL BY CULVERT VOLUME (CF) OUTPUT (CF) INPUT (CF) EXCHANGE WALLIS SANDS MARSH Culvert #1 232,319 29,760 0 0 Culvert #2 102,382 11,331 0 0 Culverts #3A 104,980 6408 6228 6 and OB Culvert #4 creeks only 543,827 85,184 71,179 13 creeks & surface 1,724,780 85,184 71,179 4 PHILBRICK BROOK MARSH Culvert #11 72,963 4892 420 0.6 Culvert #10 195,122 75,337 59,170 30 Culvert #9 creeks only 207,822 152,298 41,999 20 creeks & surface 391,180 152,298 41,999 11 5 runoff for storms of various magnitudes. In addition to storm magni- tude, factors must likely to affect peak runoff are the size of the watershed, predominant soil types, and degree of development (especially paving). In Table 3, HEC-1 results are given for 10-year, 50-year, and 100-year storms, each of 24-hours duration. For each storm the esti- mated peak runoff (given in cubic feet per second) that can be expected to pass through each culvert is given for existing and hypothetical conditions. Existing structures are further evaluated according to the level of the tide at the time of peak runoff. Low tides mean greater marsh volume is available to store runoff, hence flooding will be less severe. Conversely, moon high tides (i.e., spring tides) fill the marshes to 5.0 feet or more. If peak runoff occurs during moon high tides, salt marsh areas are unavailable to store runoff, and local flooding results. Hypothetical conditions include runoff estimates with the proposed modifications in place ("proposed structures"), and the scenario of "no structure". The "no structure" scenario is simply a basis for comparing existing and proposed conditions with an estimate of runoff assuming no roads, culverts, or other structures were in place (i.e., an unmodified, it natural" system). Perhaps of greatest interest in evaluating flooding are the estimates for "high elevation" listed for both the Wallis Sands and Philbrick Brook study areas. These numbers represent flood elevations, in feet above NGVD, for points furthest inland along each marsh's drainage. This is the maximum flood elevation expected under each scenario, because drainage of runoff from inland portions of the marsh 'A is restricted by downstream backup of flow. 6 Ila TABLE 3. REC-1 STOP14WATER RUNOFF EVALUATIONS FOR SEVERAL SCENARIOS OF' STORM MAGNITUDE AND TIDE LEVEL FOR THE WALLIS SANDS AND PHILBRICK BROOK SALT MARSHES, RYE, NH. RYE MARSH EVALUATION PEAK STORNWATER RUNOFF (cys) 14 YEAR. 24 HOUR STORM 50 TZAR, 24 HOUR STORM 100 YEAR, 24 MR STORM No EXISTING STRUCTURES PRoposto STR UCT URES No EXISTING STRUCTURES PROPOSSO STRUCTURES No EXISTING STRUCTURES PROPOSZD STRUCTURES STRUCTURE STRUCTURE STRUCTURE LOU HOOK HIGH LOW MOON HIGH LOW MOON HIGH LOW MOON HIGH LOW MOON HIGH LOW MOON HIGH SITE TIDE ?log TIOR TIDE TIDE TIDE TIDE TIDE TIDE TIDE TIDE TIDE WALLIS SANDS CULVERT 1 24 37 10 36 24 36 As it 42 26 43 CULVERT 2 a a 12 12 12 12 It 13 13 is is 13 WALLIS ROAD 67 51 60 $a 52 110 82 too 93 86 131 97 121 Ila 121 CULVERT 3 32 30 29 21 is $a st so 52 58 71 70 70 60 70 CONCORD PT. 126 70 60 77 75 212 sit 106 132 133 231 148 131 159 177 HIGH ELEVATION (FT) 5.7 7.1 5.0 7.0 6.3 7.6 5.6 7.1 6.7 7.9 6.0 7.9 PHILIRICK BROO1 CULVERT It 3 2 1 3 2 4 CULVERT to 12 to 10 12 11 19 17 16 17 16 21 so to 10 19 CULVERT 9 56 44 st so 41 97 64 34 66 61 116 99 63 77 91 CULVERT 2 56 At 33 so 39 97 60 21 66 39 116 RYE HARBOR 72 36 77 74 72 44' 23 61 23 121 73 1) as 33 144 87 27 94 As HIGH ELEVATION (FT) 5.8 8.7 4.8 714 6.7 9.8 5.9 8.4 0.5 8.9 7.2 8.4 In evaluating these data, it is important to recognize that the numbers represent predictions of a model, not actual measurements. Actual flood elevations may vary, especially if storm tides exceed moon tide elevations. Actual measurements of high elevations in inland areas for the 100-year storm of February 1978 were in the range of 7.3-9.9 feet NGVD (Gadoury 1979) 8 3.0 RECOMMENDATIONS 3.1 OVERVIEW Topographic and hydrologic evaluation of the Wallis Sands and Philbrick Brook marshes has revealed four interacting factors contrib- uting to salt marsh degradation. These are: 1) inadequate and poorly placed culverts under roads for channeling baseline freshwater flows out of marsh basins, 2) inadequate and poorly placed culverts that restrict tidal flooding, 3) clogged and inadequate tidal creeks for channeling water between culverts, and 4) man-made features on the marsh surface such as stone walls and dredge spoil that hinder surface drainage. In addition, culvert and creek inadequacies contribute to poor removal of runoff and flooding during storm events. Maps I and 2 show the Wallis Sands and Philbrick Brook study areas, and the locations of culverts examined in Phase I. To develop recommendations for improvements, tidal exchange for salt marsh restoration and stormwater management were first con- sidered separately. Improvements to meet each objective were then proposed, and integrated to develop a draft plan to meet both objec- tives. Finally, consideration for impacts*due to coastal flooding were incorporated into the final plan presented here. Drainage improvement recommendations are targeted toward restoring favorable conditions for the recovery and maintenance of the salt marsh community, and improving stormwater runoff through the marshes to reduce adverse impacts to roads and properties due to flood- ing. These objectives are generally compatible: increased pipes and channels that improve tidal flushing also provide improved stormwater management under most circumstances. Salt marsh restoration and flood protection objectives may be incompatible, however, when high tides and storm surge flood the marshes during a storm event. In such instances the storage capacity of marsh basins may be exceeded by tidal inputs. 9 East Rye Pond VI.- Ak Parion's Creek"-i Marsh 3-A Atlantic Ocean 3-B Wallis Sands ConcordPoint Wallis Sand s Watershed ek Massacre Cre Marsh,-, - - .00 A 5 MaPl- Wallis Sands Study Area. Points examined for tidal resrictiOns are circled and numbered. 10 Rye Harbor lp=d Locke Fs Neck Philbrick 10 Brook Marsh J^% Philbrick Brook Watershed Atlantic Ocean CIaNe Road Jenness Beach Map 2. Philbrick Brook Srudy Area. Points examined for tidal restrictions are circled and n=berrd. Additional inputs from stormwater or snowmelt may then result in serious flooding in low-lying areas. Based on records of the February 1978 storm (100-year frequency tidal flood), flooding due to storm surge may reach 10.0 ft. NGVD in areas surrounding Rye's salt marshes (Gadoury 1979). This is a foot higher than the 100-year flood level estimated for the Flood Insurance Rate Maps (FIRMs), based on 1976 data (FEMA 1986). Absolute protection against flooding of this magnitude is not presently compatible with existing development, or the Town's objective of salt marsh restoration and maintenance. Existing development in Rye's coastal zone occurs below 10.0 ft. in many areas, most of which in-I are subject to flood hazard under present drainage and tidal conditions. Roads built across marshes below this elevation offer little protection to landward areas because they can be over-topped by flooding. It follows that modifications of drainage structures passing under such roads cannot significantly reduce the risk of tidal flooding inland. 4 Further, anticipated rates of sea level rise indicate a high likelihood that coastal flood hazard will increase significantly over the next 50 years (Hoffman et al. 1983). Full protection of such areas may require more sophisticated structural solutions and an active management pro- gram. These prospects are leading some coastal areas to propose develop- ment limitations in anticipation of sea level rise (LIRPB 1984). Planning is currently underway in New Hampshire to provide for flood protection and marsh preservation (Shevenell Gallen 1987, D'Agostino 1988). Thus, a long-term plan for maintaining the Wallis Sands and Phibrick Brook salt marshes (and other salt marshes in Rye) must be but one component of a coastal management plan. This plan might consider such issues as road relocation and modification, existing and future development, and water control structures in light of the continuing rise in sea level. 12 Such a management plan is obviously beyond the scope of this study. However, coastal flooding and sea level rise must be considered in the course of recommending drainage improvements. To meet the objectives of this study, improvements are recommended that will: 1) improve tidal exchange to encourage marsh restoration, 2) improve stormwater removal under most circumstances, and 3) not increase, and perhaps decrease, the risk of tidal flooding during extreme events compared to existing conditions. 3.2 DRAINAGE IMPROVEMENTS The following specific recommendations are made for improving tidal exchange and stormwater removal in the Wallis Sands and Philbrick Brook salt marshes. Place names follow Simpson (1986); and previous reports by Normandeau Associates Inc. (NAI 1986a, NAI 1986b). Recommended improvements are given a priority rating of "H" (high), "M" (medium), and 'T' (low), for each stated objective. Thus, an improvement that is critical for salt marsh restoration may have a rating of "H" for improving tidal exchange. However, its importance to stormwater runoff may be quite low and thus rate 'T' for that objective. In general, improvements that will affect a large area are rated "H", while smaller-scale improvements are rated "M" or "L". Stormwater and flood protection improvements are all given high priority ratings. General Specifications: A 1) Culverts should be installed with minimal slope, not less than .002 ft/ft, positive seaward during outflow. This will encourage self-cleaning toward the seaward end during outflow. 2) All elevations are given relative to NGVD- 13 3) Improve and extend marsh ditches as specified following the typical section given in Figure 3. A rotary ditcher attachment, which broadcasts spoil over the marsh sur- face, is recommended for ditch digging. 4) Spoil material removed by means other than the rotary ditcher should be disposed of on upland areas. 5) Low ground pressure (LGP; PSI 5 2.0) equipment is recom- mended for any work requiring operation on the marsh surface. 6) Work requiring operation of heavy equipment on the marsh surface should be performed during October-April to avoid adverse impacts to salt marsh vegetation, peat structure, and wildlife. 7) All work in salt marsh areas should be performed in consultation with a salt marsh specialist. A minimum of three reviews are recommended: 1) review of final construction drawings, 2) review of work during construc- tion, and 3) review following construction. 8) Self-regulating tide gates of the type designed by Nekton Associates, Inc. of Fairfield, Connecticut (Tom Steinke, Sr., President), or similar, are recommended. WALLIS SANDS MARSH Site: Culvert #1 Recommendation #1: Replace existing culvert with 19" x 30" RCP set at approximately 4.0' invert elevation. Extend new pipe approximately one foot beyond existing culvert at both ends. Clear rocks from channel immediately south of culvert (Figure 1, see Map I for location). Rationale: Improve stormwater runoff capacity (H). Maintain East Rye Pond as brackish pond. Site: Culvert #2 Recommendation #2: Maintain existing culvert. Extend and improve existing ditches north and south of Culvert #2 (Figure 2) such that a continuous open channel exists between Parsons Creek and the marsh basin served by Culvert @J2. Optional: Install self-regulating tide gate to protect against tidal storm surge. However, low profile of road provides only minimal protection. 14 EAST RYE POND FLOW 19' x 30' RCP RIP RAP 00 MARSH RD. 1@0-39 1100i F-45 CLEAR ROCKS FROM CHANNEL IMMEDIATELY SOUTH OF CULVERT PARSON*S CREEK MARSH PLAN NO SCALE MARSH ROAD ELEV. 7.03* 117-G, 19" 30- RCP (TYPJ OOL"/- MIH. ELEV. 4.0- INV. 42- PROFILE WALLIS SANDS MARSH "o CULVERT #1 NO SCALE FIGURE I 15 .01 iMPROVE S, EXISTING 10, DITCH C3 Do EYISTING1 CULVERTI CD I 0 0 0= 10, S1 PARKING '/000' ALLIS SANDS EXTEND AND STATEBEACH IMPROVE EXISTING DITCH SALT MARSH (EL. 4.S'�:) /hD loo@ P07@j R \NV@E EXISTING DITCHES Q7 3A 13 @L@EAN PARSONi EXISTIN 10, CREEK CULVE S (TIDAL) ADD TIDE ATE 3B .(SELF-REGULATING) S, ROCK WALL* DITCHES IMPROVE ,/ENISTING- DITCH@ Figure 2. Recommended improvements for northern part of Wallis Sands salt marsh, Rye, NH. 16 Rationale: Improve tidal exchange (M). Minor protection against tidal storm surge (optional). Site: Culvert #3A Recommendation #3: Clean existing culvert. Improve existing ditches east of Ocean Blvd., especially the ditch extending south to Culvert #3B (Figure 2). Install self-regulating tide gate over west end of pipe. Rationale: Improve tidal exchange (M). Protect against tidal storm surge (H). Site: Culvert #3B Recommendation #4: Clean existing culvert. Improve existing ditch between culvert and Parsons Creek to the west (Figure 2). Install self-regulating tide gate over west end of pipe. Rationale: Improve tidal exchange (M). Protect against tidal storm surge. Site: Wallis Road Vicinity (Culvert #4) Recommendation #5: Relocate creek in vicinity of Horse Paddock and Trash Corner (Figure 5). Follow detail given in Figure 4. Rationale: Improve tidal exchange (H). Alleviate erosion and encroachment problems at Trash Corner (H). 4 Recommendation #6: Deepen existing creek in the vicinity of Wallis Road by approximately 1.0 ft., to a bottom elevation of approximately 2.5 ft. (Figure 2). Rationale: Improve tidal exchange (H). Recommendation #7: Remove remnant of Old Wallis Road roadbed from creek channel (Figure 5).' Follow detail given in Figure 6. Rationale: Improve tidal exchange (H). 17 3 0- ARSH SURFACE 4.5':t 3 30" -SPOIL BROADCAST OVER MARSH SURFACE USING ROTARY DITCHER lo.. TYPICAL DITCH SECTION NOT TO SCALE FIGURE 3 10, A 4.5't FILL FROM NEW > E XCAVATION 3 al@ 3.5'2: 2.5't 9.3' RELOCATED CHANNEL EXISTING CHANNEL SECTION E E' NOT TO SCALE N@3 FIGURE 4 18 �ONS CREEK (17DAL) S, --OHO RSE PADDOCK 10, "TRASH, I RELOC CORNER" CREEK DEEPEN EXISTING CREEK%, BY 1.0- t: 00 DEEPE* \ EXISTING \51 0 CREEK Ak"w, BY 1.0't REMOVE S, 10, REMAINING ROADBED I ZZz@@ FROM WOODED CHANNEL 10, UPLAND R Figure 5. Recommended improvements for Wallis Sands salt marsh in the vicinity of Wallis Road, Rye, NH. See Figures 6 and 7 for section details. 19 REMOVE ROCKS TO 3.2*t PROVI DE SMOOTH SLOPE ROCKS -ZPROPOSED SLOPE OLD WALLIS ROAD ROADBED SECTION A - A'. NOT TO SCALE ROAD BED G.O,� 4.5'illLtu STONE k-MARSH FOUNDATION -3.2*� ROCKS TO BE REMOVED 0-1.0,2 LPROPOSED- BOTTOM OLD WALLIS ROAD ROADBED SECTION B - B' NOT TO SCALE @F L t RO F B E FIGURE 6 20 Site: Culvert #5 Recommendation #8: Maintain existing culvert (Map 1). In the course of a routine replacement program, replace with similar capacity pipe set approximately 0.5 - 1.0 ft. below existing invert elevation of 3.5 ft. Rationale: Improve tidal exchange (L). Site: Concord Point Outlet (Map 1) Recommendation #9: Maintain channel free of sediment and organic matter buildup. If possible, remove barge remnants and reconfigure channel as previously specified. Rationale: Improve tidal exchange (H). PHILBRICK BROOK MARSH Site: Culvert #11 Recommendation #10: Replace culvert with 24-inch RCP set at approximately 3.5 ft. Improve and extend ditches east of the pipe (Figures 7 and 8) to create a 6-foot radius, semicircular basin at the pipe mouth, with drainage ditches extending north and south from the basin at the foot of the highway embankment. Rationale: Improve tidal exchange (M). Site: Culvert #10 Recommendation #11: Replace existing culvert with 29" x 45" RCP set horizontally at approximately 2.5 ft. (existing CMP is at approximately 3.0 ft.). Improve existing creek by removing sediment deposits east of pipe (Figures 7 and 9). Rationale: Improve tidal exchange (L). Site: Culvert #9 Recommendation #12: Replace existing culvert with 29" x 45" RCP set at approximately 2.0 ft. Improve existing creek by removing sandbar south of pipe, and rocks and peat chunks north of pipe (Figures 10 and 11). Rationale: Improve.tidal exchange (H). 21 Lik, Jjk'1 loll 10 REPLACE %% AS .... % SPECIFIED % CLEAN ROCKS and SEDI VP MENT k-, FROM CREEK UPLAND 01 10, SALT MARSH 0 EXTEND AND 50 IMPROVE EXISTING DITCH and BASIN 10, REPLACE AS SPECIFIED UPLAND 151 \CLEAN 1 CREEK I TO CULVERT Figure 7. Recommended improvements for southern part of Philbrick Brook salt marsh, Rye, NH. PHILBRICK BROOK SALT MARSH FLOW RIP RAP RT IA OCEAN BLVD Db EXTEND AND IMPROVE E)asnNG DITCH AND BASIN PLAN NO SCALE RT. IA OCEAN BLVD. ELEV. 9.00' 24- RCP (TYP.) .002% MIN. - - - - - - - - - - - - - - - - ELEV. 3.5' INV. 90, PROFILE PHILBRICK BROOK MARSH 0 voo CULVERT #11 NO SCALE FIGURE 8 23 PHILBRICK BROOK FLOW PRIVATE DRIVE RIP RAP CLEAN ROCKS AND PLAN SEDIMENT FROM CREEK NO SCALE EAST OF PIPE PRIVAIE-DRIVE ELEV. G.85* (TYFJ 29' x 45" RCP SET HORIZONTALLY ELEV. 2.5* INV. 40' PROFILE PHILEIRICK BROOK MARSH CULVERT # 10 NO SCALE A FIGURE 9 24 U EO 'EXTEND ANDI CEXTEND. IMPROVE Of AXISTING DITCHES EXISTING DITCHES of Lj %TIDAL of REE 1 NEW ROCII I - WALLS ITCH SALT MARSH (EL. 4.S'�) Ln EXTEND 80 /DITCHES FROM I CREEK of EXTEND CLEAN ROCKS and IMPROVE CULVERTS 1 7, 8, and 9 I SEDIMENT [3 AS SPECIFIED FROM CREEK NEW) 10, 9 - DI I Figure 10. Recommended improvements for northern part of Philbrick Brook salt marsh, Rye, NH. REMOVE EXISTING ROCKS AND PEAT CHUNKS NORTH OF PIPE \--GRANITE ABUTMENT 29' x 45- RCP LOCKE RD. REMOVE EXISTING SANDBAR SOUTH OF PIPE FLOW PLAN NO SCALE LOCKE RD. ELEV.'7.68' 101-6" GRANITE ABUTMENT po (TYP.) - - - - - - - - - - - - - ELEV. Z.00* INV. 40* -- ------- @SELF-REGULATING TIDE GATE ON NORTH END OF PIPE 29- 45- RCP PROFILE PHILBRICK BROOK MARSH CULVERT # 9 (TYP.) NO SCALE FIGURE I I 26 Site: Culvert #8 (Granite sluiceway) Recommendation #13: Replace existing sluiceway with similar structure approximately 48 inches wide with same invert elevation. Install self-regulating tide gate at east end of sluiceway. Rationale: Improve stormwater runoff capacity (H). Improve tidal exchange (L). Protect against tidal storm surge (H). Replace deteriorated structure. Recommendation J114: Dig new ditch from tidal creek near west end of Culvert #8 southeast into panne area (Figure 10). Rationale: Improve tidal exchange (L). Recommendation J/15: Improve and extend existing ditch from vicinity of west end of Culvert #8 southwest through panne areas and existing stone walls (Figure 10). Rationale: Improve tidal exchange (M). Site: Culvert #7 Recommendation #16: Extend and improve existing ditches west of Ocean Blvd to pass through existing rock walls and intersect panne areas (Figure 10). Install self-regulating tide gate at east end of pipe. Rationale: Improve tidal exchange (M). Protect against tidal storm surge (H). Recommendation #17: Dig new ditch from vicinity of east end of Culvert #7 south into panne area. Extend ditch through panne area for maximum effectiveness. Locate ditch in the marsh, as near as practicable to the base of the highway embankment (Figure 10). Rationale: Improve tidal exchange (M). Site: Marsh South of Rye Harbor Recommendation #18: Extend ditches from existing creek in southern part of marsh through stone walls and into panne areas (Figure 10). , Rationale: Improve tidal exchange (M). 27 Recommendation #19: Extend existing ditch east of main tidal creek near Harbor Road bridge east into panne area (Figure 10). Rationale: Improve tidal exchange (L). 28 4.0 LITERATURE CITED COE. 1980. New England Coastline Tidal Flood Survey. U.S. Army Corps of Engineers, Waltham, MA. D'Agostino, S. 1988. Wetlands: Victims of sea level rise? Coastal Planning Newsletter, New Hampshire Office of State Planning, Concord, NH. Federal Emergency Management Agency (FEMA). 1986. Flood Insurance Rate Maps, Town of Rye, New Hampshire, Rockingham County. Community- Panel Numbers 330141 0002B and 330141 0003B. HEC-1. 1985. Flood hydrographic package (IBM XT 512K version). U.S. Army Corps of Engineers, The Hydrologic Engineering Center, Davis, CA. Hoffman, J.S., D. Keyes, and J.G. Titus. 1983. Projecting future sea level rise. Methodology, estimates to the year 2100, and research needs. U.S. EPA Office of Policy and Resource Management. Washington, DC. EPA 230-09-007. 121 pp. LIRPB. 1984. Hurricane Damage Mitigation Plan. Long Island Regional Planning Board, Hauppauge, New York. 196 pp. Normandeau Associates Inc. 1986a. Phase 2 Report. The Coastal Wetlands Mapping Program, New Hampshire. Prepared for the New Hampshire Office of State Planning Coastal Program. Normandeau Associates Inc. 1986b. Tasks 2 and 3 Final Report. Summary of field investigations of coastal wetlands and associated road crossings in the Town of Rye, New Hampshire. Prepared for the Town of Rye and the New Hampshire Office of State Planning Coastal Program. Shevenell Gallen and Associates, Inc. 1987. Technical Report. Rise in Sea Level and Coastal Zone Planning. Prepared for Office of State Planning, Concord, NH 19 pp. Simpson, M. 1986. Restoration of Parsons Creek Marsh, Rye, NH. Antioch New England, M. Sc. Thesis. 29 I NO ST SERVIII S CTR LIBRARY I @ii lillill 1 3 666 141 1867 1 1 I I I I I 0 8 a 61 AL. CE lll@@ llll@ 8 1