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HomeMy WebLinkAbout20080868 Ver 2_Section I D - G Drought Storms Rainfall Discharge_20210701Table I-C-1. Estimated historic and current drainage basin of each control and impact creek in the study as described in CZR 2011 (PA2, Little Creek, Long Creek, Duck Creek, and DCUT19), in CZR 2017 (SCUT1 and Broomfield Swamp Creek), and in previous annual creeks reports (Jacks, Jacobs, Drinkwater, Tooley, and Porter creeks, Huddles Cut, and DCUT11). Permitted impacts to all NCPC creeks north of Highway 306 have been completed; after permitted impacts are completed in the Bonnerton Tract, the mine will move into the South 33 Tract and Broomfield Swamp Creek will have permitted basin reductions. (Estimate sources: USGS topoquads, LiDAR, USGS stream stats https://streamstatus. usgs.gov/ss/) Control creek Drainage basin Basin land use Historic (ac) Current (ac) Reduction (%) SCUT1 - 1,965 0 Agriculture Little Creek 1,822 1,722 5 Agriculture Long Creek 630 223 65 Natural vegetation PA2 - 22 0 Natural vegetation Duck Creek 3,118 3,118 0 Silviculture; agriculture DCUT19 121 121 0 Agriculture Impact creek Broomfield Swamp Creek - 1,946 0 Agriculture Jacks Creek 645 150 77 Natural vegetation Jacobs Creek 751 202 73 Natural vegetation Drinkwater Creek 605 153 75 Natural vegetation Tooley Creek 563 257 54 Natural vegetation Huddles Cut 1,014 289 71 Natural vegetation Porter Creek 3,745 840 78 Natural vegetation DCUT11 166 81 51 Natural vegetation Note: Due to heavy agricultural use and flat topography, SCUT1 and Broomfield Swamp Creek historic basins have not been estimated and are presumed to not be significantly different than what the USGS stream stats web tool calculated; CZR biologists verified flow direction in all contributory ditches in both basins in 2017. PA2 was excavated from uplands between Jacobs and Drinkwater creeks and therefore had no historic basin. Muddy Creek (control) is monitored only for fish/benthos and sediment/water column metals; its basin is amongst the largest of the creeks in the study and land use is predominantly silviculture and agriculture. Durham Creek (control) is monitored only for depth and salinity at one location, has the largest basin, and land use is mixed between natural vegetation, silviculture, agriculture, and other human development. I-C-4 D. Drought Drought conditions are monitored nationally by several indexes. The US Drought Monitor (http://droughtmonitor.unl.edu) provides a synthesis of multiple indices and impacts and reflects the consensus of federal and academic scientists on regional conditions on a weekly basis (updated each Thursday). Reported drought conditions in the study areas located on the south and north sides of the Pamlico River were summarized for the years 2000-2005 and 2007-2020 (Table I-D1 . drought data begin in 2000). For study creeks on the south side of the Pamlico River, 2002, 2007, and 2008 were the driest years reported, with 77, 79, and 81 percent of weeks with some drought classification. On the south side, years 2000, 2003, 2004, and 2015 had normal conditions during those entire years (Table I-D1). The driest year reported on the north side of the Pamlico River was 2011 when 28 weeks (54 percent) of the year were assigned some drought classification (Duck Creek data include 2010 through 2020). On the north side, 2015 and 2018 had the least amount of weeks with a drought status. While there was some variation in annual patterns of rainfall or drought status between the two sides of the river, when only the data years in common for both sides of the river are considered (2010-2020), each side had an average of 41 weeks with no drought status. No years included in the summary table have been considered in extreme or exceptional drought on either side of the river. I-D-1 0 k w \ y �fcJo CV'( G 220 ) o e o_ 0- % Io o\- k / I ] .a > o o \ / 3 § 2 E I 0 a 0 2 — 2 § £ / § ( a) 7 9 e c3)\/f �-o 0 2 _ 2 7 2 ® / ¥ 0 % 2 / .> 0)o 0) I E £ 2 a) = c c a) as co /-¥ C5) ) 2 E v .s o2/ 8 9 \ 2 = .g22& o a) -aa) a) a) ED I % _ E a * £ / \ OD/y% 0 0)- k�oZ " 0 2 0 k :Ifo £ £.k_ ' cm%±.S 2 * / 2 E E 2 D E O./ Percent of Weeks with a Drought Classification 28 20 Exceptional Drought (D4) 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 Extreme Drought (D3) 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 Severe Drought (D2) o e N.- 0 0 0 e w 0 0 2 0 0 0 0 0 0 0 0 0 0 CO0 0 0 0 0 0 0 0 0 x- Moderately Dry (D1) o N-m 0 0 0 e R a n» R 00 0 0 0 0 0 0.7 n» e 0 0 0 0 0 0 0 0 01 Abnormally Dry (DO) No Drought Status G m e G O 2 R R 3 m m g G$\§ Q§ 37 R a m§ OIg g cr / 0 0 0 0 0 0 a a a a a a 0 0 000000 000000 a a a aa a a a a a a 0 Ave rage 000000 0 0 0 0 0 aa a a a a a a a a Ave rage Location j./� _\y §$/E -0 {/ /qa� {! § G= a- 0 * -8 35» pD 2 E. Extreme Events or Storms Event dates, types, and descriptions of extreme events or storms in Beaufort County that could have affected rainfall, hydrology, and/or salinity data collected during 1998-2005 and 2007-2020 were gathered from the National Oceanic and Atmospheric Administration's (NOAA) National Climatic Data Center (NCDC) Web site (Table I-E1). Event types selected for Beaufort County in the Storm Events Database included: Astronomical Low Tide, Blizzard, Coastal Flood, Drought, Excessive Heat, Extreme Cold/Wind Chill, Flash Flood, Flood, Heavy Rain, Heavy Snow, High Wind, Hurricane (Typhoon), Storm Surge/Tide, Strong Wind, Thunderstorm Wind, Tropical Depression, Tropical Storm, and Winter Storm. Event types were selected based on likelihood of affect to rainfall, hydrology, and/or salinity data. Some events are not shown in the table if they were repeat data. For example, if a Hurricane and a Storm Surge/Tide event were on the same date, the Storm Surge/Tide event was left out of the table. Events that may have been severe in other counties of North Carolina, but were minor in Beaufort County, are also not shown. Hurricanes and/or tropical storms were the events most likely to affect the data. Over the years of the creeks study, there have been 11 hurricanes and eight tropical storms that have affected the area. Hurricanes and tropical storms that switch categories are counted as one event. Other extreme events reported over the years were heavy snow/winter storms, high winds, flash flooding, and severe drought. There were seven recorded extreme events in 2020. On 20 February a low pressure system produced showers that changed to snow towards the evening in Beaufort County. The amount of snow that fell was estimated to be 2 to 4 inches across Beaufort County. Thunderstorms on 6 April, 18 April, 30 April, and 1 August produced damaging winds throughout Beaufort County. The final event for 2020 was Hurricane Isaias which was rated a tropical storm in Beaufort County. This storm brought winds up to 60 mph and 2.5 inches of rain. I-E-1 a) a a H c w Winter Storm co O c 7 3-5' of rain across region caused Tar River to crest over 18 feet; flooding occurred in Belhaven and Washington. Winter Storm c c) m O c D U E a) a3 a) O O c D O O N O U a) O c O TD c O Co O Q Winter Storm co 0) O a) LL L a E Thunderstorm Wind co V ai E D c D N Q a) D O c U D O Q L 0) a) O E a) c 0) ( O L U a) 0 0 ( N a3 U a3 s E a) N T Thunderstorm Wind A squall line across eastern areas of the state produced baseball size hail and wind gusts between 60 and 70 mph. Thunderstorm Wind CO co co O ca c N N Hurricane Bonnie brought 7-10" rain which resulted in some flooding in some areas. a) c co 0) O 0) Q co L Q E co co O a N O a) a) U D O Q D c E N a) D c 1- Thunderstorm Wind O 0 Thunderstorm winds produced gusts up to 63 mph. Thunderstorm Wind a) c O O 0) Q co (0 E O c O a3 N v to O N a) c N O >, (0 0 C o Z a) c 0 O 0 o 0 0 a) m D c a) O a3 N 0 0 0 > O LO a) rainfall recorded was a) c E O 4- a) 0) 0 0 0 n a3 0 D N ( 'p a) o 3 LL s TD aa)) (o > c a) O ao N C c 'S U ID a) N 2 a) a3 C E c D U U O 0) c D 0 0 0 D LL D c a3 to c c a) 0 a) a) c c as as U U estimated at 4-6" with some Irene rainfall a) c O 0 0 Average of 6 inches of snow across Coastal Plain. Reports of 9 of 13 inches were not uncommon. 0 c a) O_ O_ O_ O_ O_ EEE EE co co co co co O O O O O o_ o_ o_ o_ o_ mmm O O O O O (1) (1) (1) (1) (1) 0 0 0 0 0 0 0 0 0 0 O O O O O O_ O_ O_ O_ O_ o o 0 0 0 c c c cc EEE EE `O `O `O be) N N N N N 0 0 0 0 0 c c c cc m m m Thunderstorm Wind Thunderstorm Wind Thunderstorm Wind O O O O 0 a) 0.5 n F co Thunderstorm Wind Thunderstorm Wind 0 c U) 4 to 8 inches of snow in Beaufort County. Winter Storm Thunderstorm winds produced gusts up to 63 mph. Thunderstorm Wind Oco O 7 Li N N c a) • N a) • O t O O U O O _c U_ E TD Ll N _C N 0 -o a) E o 0 0 S a) a) E co `0 O N � a3 0 N io E U a) m m Y > c N a) m wc to (rE O a) O co > a3 c a) 0 4- c E (0 _0 O N a) U (6 c 0 (0 S Z a) c I-E-2 Table I -El (continued). Event Description Wind gusts 50 to 72 mph. Thunderstorm winds produced gusts up to 60 mph. Several severe thunderstorms produced winds gusting from 50-90 mph. total of 6 to 8 inches of rainfall. Remnants of Tropical Storm Tammy. Several storms produced large hail with wind gusts up to 60 mph. Thunderstorm Wind a) (13 0 U 7 2 Tropical Storm Thunderstorm Wind a) (13 0 U 7 2 Flash Flood U Thunderstorm w cc O r 0 C Le) N O W Ln O Q a) O 0 W O O) 0 U a) 0 O Q N N a3 O U c C O a) C O U C a3 t Q E co O Q O) C N 0 C C a) U 0 0 O Q N E O N a) a) 0) Several severe storms produced large hail and wind gusts up to 60 mph. O O Q O U C U - 00 0 Q c w a) 3 C O U C O N rn c a) 0 Q U C a3 N a) a)) a) E O N C O)o -O C N a) N OS N O c C Q E O 2 O a) w Lo 0 a) a) 7 _c N 4) () m U U U a) 00 C 0 Q 0) the Pamlico River in Washi _c w C a3 a)� 2 E c O w N U OS a) 0- 0) CO 0 . O Bands of showers across eastern North Carolina produced wind gusts up to 60 mph. Several severe storms produced large hail and wind gusts up to 70 mph. 4 to 7 inches of snow. Scattered thunderstorms produced wind gusts up to 60 mph. Scattered thunderstorms produced wind gusts up to 60 mph. Rainfall total 6 to 8 inches. Significant flooding in low lying areas and along small streams, especially in Washington. Scattered thunderstorms produced wind gusts up to 60 mph. Carolina. Several across eastern North largest tornado outbreaks ever observed One of the warning area. had been well below normal. had been well below normal. A series of weak upper level disturbances produced wind gusts up to 60 mph. One small tornado was reported. U Thunderstorm U Thunderstorm Tropical Storm Thunderstorm Wind Thunderstorm Wind Thunderstorm Wind Thunderstorm Wind Thunderstorm Wind Thunderstorm Wind O) O 0 O) O 0 O) O 0 a) (13 0 U 7 2 Thunderstorm Wind O Ln 0 C N co Q a) co O C r 0 C N O a) a) LL N th 0 N 0 r O Q a) co N Ln (.6 Q a) co N I-E-3 Table I -El (continued). Event Description Several severe thunderstorms similar to a derecho produced hail and wind gusts up to 70 mph. Several severe thunderstorms produced large hail and wind gusts up to 60 mph. Several thunderstorms produced wind gusts up to 60 mph. A severe thunderstorm produced damaging wind gusts up to 60 mph. Snow mixed with freezing rain at times. Total snow accumulations were 3 to 5 inches across the county. changed to rain. C 0 0 CO U) CO N 0 O t a) C c E m a) a) a) CO C c C O co t 0 z Numerous showers and isolated thunderstorms crossed eastern approached from the west. Heavy rain led to some flooding in Beaufort County. and large hail. Persistent showers and thunderstorms led to rainfall amounts of over 3 inches across central Beaufort County. E a) t U m O Q Q (6 C O U m U) (6 rn c c aa)) a) a) C CO (6 C c O CO m 0 ( c a) C 0) CO co o a) C U 2 Q a) a) U) a) E co U Q U) E O N a) 0 t O C a) eastem North 0) c O m U) c O co U O T C (6 E C a) n a) a) N O Q a) a) C (6 T C 0 0 CO CO a) a) C O U E (6 d 0 7 O a) (6 1 O t Q E N 0 0 aj -D C a) N 9 O a) d _c Up to 4 inches of snow fell in Beaufort County; PCS Aurora recorded a lesser amount. (1: t n U t (13 • t m a"' a) O C • • Z o _c co co 0 D 0 0 U) a) -D O U a)) co 0 d > c U > O 0 (6 -O U O c O N a) a) 2 a O E U .— N U) Q C O N U) Q a) N 0 Q 2 0 (6 N U co O O H -o lone to ever make landfall in the Storm Ana was the earliest Thunderstorm winds produced gusts up to 60 mph. t Q E O c co c N a) a) co d (6 a) t N cri (6 (6 a) 2 O tc W co To (6 a) U 0 Scattered thunderstorms produced hail and wind gusts up to 60 mph. 7 inches associated O Rainfall totals in: to 3 feet above Thunderstorm Wind Thunderstorm Wind Thunderstorm Wind Tropical Storm Thunderstorm Wind Winter Storm Winter Storm O O LL Thunderstorm Wind O O LL Thunderstorm Wind Winter Storm Tropical Storm Thunderstorm Wind Winter Storm Thunderstorm Wind Tropical Storm a) cc () N N 0 00 N co 00 N co a) a) LL 4 N (13 0 N co a) a) LL co co N co co () N I-E-4 Table I -El (continued). Event Description October 9th. Widespread t 0) 0 O October 8th C 0 Carolina coast late moved offshore of the c a) t U 0 O 0 O_ a) a) t U) t 0) a) Q 0 U 0 C 0 > a) a) 0) 0 0 Z a) c C c 0 0 C CO t W Q 0 U 0 C 0 a) O_ 0 aa)) C c6 U) t Hurricane Matthew moved northeast offshore of the a) C 0 U op rn cci c6 0 E 0 N t > C 0 0 a) O U) a) t U C 0) 0 co > a) c a) c C c (6 c U) a) t U C N 0 W 0 on the southern beaches rain led to significant flash flooding over much of eastern North Carolina during the inches reported northwest of Washington. Thi a) a) 0 0 O E most main -stem rivers exceeded 1- t N 0 0 U) 0 t 0) C c 0 E >, .OS 0 (1) 0 a) C C -0 0 CO c C 2 (73 (6 U c to U) z E a) -0 o o w t U) 03 O 2 m 0 IQ _C a) CO -° 0 O a) -0 c a) m N U) U) .C_ >, U) w U) 3 N p) O 0) o 2 To OS 0 0 U -0 O cQ O c U1 O Q w Flash Flood An isolated severe thunderstorm produced large hail and strong wind gusts up to 63 mph. Thunderstorm Wind Several severe thunderstorms resulted in wind gusts up to 63 mph. Thunderstorm Wind a) cc 8-12-Oct-16 0 Q N 0 N 0 hazardous winter weather across eastern North U) c C O U) a`) t a) a) C a) iTs C 0 C N O_ U c a) O o 0_ 0 C a) m E U O C) E C a) m o c _c O ¢ +.-. 0 co M ° L, U a ._ 9 - E U) 0 U) N p) O . C c6 O a) U c I) -c •C _c a) Eo N c E ca 2 U EtOS U o Winter Storm a) 0) c 0 CO C O U t 0 Z a) U) a) a) 0 U) 0 E O CO .N a) U 0 O O t Z 0 t U c C c U) U) a) E a) C C 0 0) a)) a) 0 0 c W CO C CO 0 c .E 0 E > a) a) a) t 0) a) O Ot N- O) N— Q (1)a) -0 4_ 0 U) U) N C O_ a) o J (6 Winter Storm Ocracoke area north to Duck along the Outer Banks. A prolonged period of strong west to southwest winds produced record low water levels in the Neuse and Pamlico rivers. Low Water Event a) U) a) 0 a) E 0 M 0 t 0) c c a) C CO 0 0 0 E a) a) C .3 c O U a _cr O Z E °- a) U) N U) CO -° a) .co c o E O Q) -0 -0 N U) O U) a) C C U) 2 a) c C 0 U) E U N E O U) a) C 1- became severe with large hail U) ( t a) 0 c 0� U) 0 �� N o 0_0 o o Ea) 0 0 E U) 0) E OS a) ° CO La _ C U) Q) '� U) '§ 0 OS C C M U) O 0) c0) Y C O ° p C (6 t (6 o m '3 a w a U N >' 0 0 o .E U) m . _C° .5 .o U) C a) 0) ~ C M U C t N 0 C Q d C E C - T.)N U) 0 o c) co coO_ °-a) N >, .- 0 N (n C E ° 0 a) -O N U N _c co O E. Q Q C a) U) 0) 3 LX) O ° > a) 'C ° _ a) U) C co c 0 ° U) C ° >, a) 0 co) E c c N U) E p 0 ° 3 N C p U) c m-C 8 N o o a) E 0 U) -O N 0) N t O ° E _c i O Zi m N °_ 0 m 3 > — 0 E 0 cl) c =° Q o 0 U) _co 3 C O M N 7 _a)a) t o .� ° Tropical Storm in Belhaven. 00 co M 17-18-Jan-18 2-5-Mar-18 OD N op 0 0 M I-E-5 Table I -El (concluded). O s 0) c c ernoon and e re thunderstorms during the a u) 0 O c O a) U o 0 O 0 c 0 0 c C E a) N > u) u) u) 0 0 O c O N and damaging winds. Scattered to numerous severe thunderstorms developed during the evening hours, producing ted through the first half fternoon hours, and I 0 0 O O E O i c c a) o- E O O -o ) Q 0 (1) O .O § O � N L O c O a) Q of the 2019 Atlantic hurricane season. (. E co a`).c D o E) m U a a) o - co •E Z N 73 E co . o c (1) a) N (o (0 ._ a) 2 c U(No s : -0 Z I ate) O a.)U (B 0 a) 0) U O C ( O "'alN 0 (o _ 0 (o 0 (o D as O O O O - O a) (B E O co > a) E N w E _T c _cN P a.) O as (Da) o ca) E •O- C 7 u) N a) o_ c -O Y oo (I)0 0 O 0 J O E 'N m L O N U o) N .g a) E r Q 0 E 5 .0 E c .E a)fn _c _c — N O o c 0 o U E a) a) os 73 N 0 L' ( O 0 LS U C N -cUO 0 Y �0 Too N m a) c a) N as U O -o O E j o O ma E o Rainfall amounts of 5 to 10 0 Q E l(i 0 0 0 u) O L Q0 E Lf) N O 0 .c U a) c a) O Q u) c C a) C N u) E XE Thunderstorm c Thunderstorm Thunderstorm Tropical Storm 0) 0 Q 0) Q (1) M ZCL vi O O 0 c c m m � Et '(m E N j 2 O cD a) c c LL 'c > i O NO a) 2 o c 0 u) O C' — O p c c a) c fir. O U ( N _ � N a) LL N .X N O E LL (o >' o c N i O co co U s - c c 'c o (o Z o a) Ot E N >, O co N i L N -O LL 2 Q0 O O -O > O O E a N ) � O U N . 0 Q u) -O H a) O E c c a) U 0 O 0 c C a) u) a) E 0 a) E O N a) c 0 O c .c a) a) 0) c L O O O E u) E 0 i a) c C c a) a) 5 EFOs, and 1 EF1. a) 0 O 0 a) E O L O c c a) > a) O c O O E a) a) O c c O O (1) a) L O a) O E c c as • u) E a) O O O N > ) -N 0 a) O O a) (L12 E o - C _c c H re thunderstorm wind reports we d through the region during the day. A couple se line moved through. < ai E a) 0 u) a) u) 0 U c c a) u) a) E 0 a) thunderstorm c m _c O c N U c u) c 0 _ u) 2 1-5 u) a) o U ccO-0 Q O i co c< (0 ( 0 c -0 s c < _� a)�'N 0 0 0sZ¢0 io (co c (o Z '(3 N D 0 0 -O O) a) N u) o a.) Z c c E . �° E -o (n CDm a) CZ (I)LE) a) a) m a--. u) LP TZ ui E a) 0 c Q E `o N C ' o m m E O i a) 0) N O D U o w E a) : 0 m e (� >+ O a) (o a)0 _00 O N O c0 a) 5' 7 L N N -0 c< N (I) O U (I)om 0 0)_ N 0 :E c (I) c �a) 0 Y 0 0 = 0_U O CO O CO E os E ( o- O 0 a�u)O cc Eaa) OU O 0) (I) o s- .ca) E _o >, aa.) a) C a) os a) o o Q (o O- C (� E N >' (n- N a)-C O N N 0 (o 0 O U 7 -O a) .0 U N 'Q O p 'i c (o (o 2 0) O N •- LS (o U O t 0 0 c co 2 c 73 0' o o c c a) 0 m .5 -O (o Q () N Y Hurricane Isaias c (o c O O U ?' O H Z O o E (`o o E ) a3i mow a)< (o ( a) 2 a) U E U co _c o_D Winter Storm E u) c 1- Thunderstorm Wind Thunderstorm Wind Thunderstorm Wind E u) c 1- Tropical Storm 0 Q 0 Q 0) Q I-E-6 F. Rainfall Monthly precipitation data were obtained from the Agricultural Applied Climate Information System (AgACIS), which is a repository for data collected at stations in the National Weather Service (NWS) Cooperative Observer Program (Coop) network supported by the Natural Resources Conservation Service (NRCS) and National Water and Climate Center, within the U.S. Department of Agriculture (USDA)(http://agacis.rcc-acis.org/?fips=37013). Monthly precipitation data from the Aurora 6 N station as provided by the USDA/NRCS/AgACIS database are identified in Figure I-F1 and Table I-F1 for years during the course of the study, 1998-2005 and 2007-2020. The WETS 30t" and 70t" percentiles are from the 30-year period of 1981-2010. The Aurora 6 N station is located and maintained in the vicinity of the PCS/Nutrien administrative building and a small private runway along the south side of the Pamlico River, about 6 miles north of Aurora. In addition to the Aurora 6 N station, there are six other rain gauges associated with the creeks study that are monitored to provide more site and basin specific data. Data from these six additional gauges are monitored by CZR and gaps from any period of a non-functional gauge are supplemented with data from the next closest working gauge. Measured onsite data from Aurora 6 N and the six additional sites represent raw measured data and are often different than data found in the AgACIS online data used to determine WETS percentiles. Data from onsite gauges are found in Table I-F2. Comparison of the USDA/NRCS/AgACIS online data with the raw onsite data show total 2020 annual rainfall for Aurora and raw measured data to be above the 70t" percentile. Online data show three months of 2020 as above, two below, and seven within the 30th and 70t" percentiles, while raw data show five months above, one below, and six within the 30t" and 70th percentiles (Table 1- F2). The rain gauges currently monitored by CZR were installed in 2010 (Tooley Creek), 2011 (PA2, Huddles Cut, Porter Creek, Duck Creek), in 2013 (DCUT19), and 2008 (SCUT1, Broomfield Swamp Creek). Prior to 2019, the rain gauge for SCUT1 and Broomfield Swamp Creek located at Bay City Farm was utilized for other projects. In 2020, the Huddles Cut rain gauge was relocated to the ferry landing approximately 1,200 feet northeast of its previous location. During the early years of the study, rainfall data at Jacks Creek, Tooley Creek, and Huddles Cut were provided to CZR by Dr. Wayne Skaggs per the agency approved plan and from CZR monitored gauges within Jacks Creek, Tooley Creek, and Huddles Cut used for the wetland hydrology analysis. Prior to installation of rain gauges in other creeks, Aurora 6 N rain data were used for rainfall and, after installation, were also used to supplement data gaps. I-F-1 16 14 12 10 8 6 4 2 0 Monthly Rainfall Totals with WETS percentiles for 1998-2020 at PCS Aurora Station 6 N • • • • • •• • ,• • • • • • ,••_ a • a • a a a ••• J a •Ai& a a • aA.. AL. • • •• • • • • • • • • • • •• •• • •• • • •••• • • • !! • .:5`b ���� � ❑g2�0)`') p Q p Al' \ Al' A0o� poh tApQtAoA� 0 �`e,(• \� ,\��9,< i1gy�sa 94•t944.t4. a�sa0�sea,o,�a�, ,,,°,° • Total Monthly Rainfall —WETS 30 Percentile —WETS 70 Percentile 14 12 10 8 6 4 2 0 • •• • • • • • • • • •• • • • • • • • •• • • ••� •�• a•• • • • • • M • •• • • A°o3dS\6sAo�tiodo,yoyododotititi`ytiti,ti�tiitititi`titititi�ti`tiptititi,ti�tiy,`Nkyj,%`tihbyyPti,ti�,ycysoti,ti°t,<.P�tib��ti�,ybtibti�,yaN7tigy9ti,ti�tio,yo yo15¢,tio19' ,V � oy Q� > oy 9 �+ � q%1 �+ o� �� �� �� JS 9 JS Q �� Q4oy �� �y Q �oe9�o a�a4b. 2. o a\a�a e o a4\ 4\ e a44\ e ❑ a�a�,a ¢ ❑ a�a�a ¢ ❑ �a� ¢ o aaa e o a44,a e o a�a�,a a4a�g e o a4aa • Total Monthly Rainfall — WETS 30 Percentile —WETS 70 Percentile Figure 1-F1. Rainfall summary across years of creek study: monthly totals at PCS Aurora Station 6 N compared to 30-year WETS rainfall. I-F-2 Rainfall (Inches) Antecedent Precipitation vs Normal Range based on NOAA's Daily Global Historical Climatology Network 10- h 4 n Jan 2020 n Fen 2020 Mat 2.02;0 n Apr 2020 r May 020 ur, r Jun 2020 Jul 2020 ti' Aug 2020 n Sep 2020 n Oct 2020 — Daily Total — 30-Day Rolling Total 30-Year Normal Range Nov 2020 Dec 2020 Figura and tabkas mada by tha Antecedent Precipitation Tool Vnrsio 1 ,) Wrttten by Jason O ten U.S. Army Colos of Engineers Start of Growing Season: March 14 End of Growing Season' November 24 Figure I-F2. Annual rainfall for 2020 Aurora 6N as determined by the USACE's Antecedent Precipitation Tool (APT) compared to preceding 30 years. 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O W (�O ((f L(j N C) C) .,,,; Lo N C) M COM M V (0 0 M M —N N O 3 c N N V C) C) (,.) ,_ V C) V C) L(j C) C) (O (30) N V C) February Off) to 0 0 N 0 (D 1.6 r- C) C) Lo 1.6 ONO C M Ln ON) ,_ M O M M CO N N r- 1.6 O L(j N N R C) V (O .— .— R N W.- N C) C) a) N V co O) O jn co r- Lo c0 cD r ^ LO 7 Lc; C) R— V _— co A V op .— I— M .— co .6 N 00 N CO coco c0 O LO O N (Np c'7 7 N (.0 CD co cD V C) N V C) N N N V C) N �' V in co co= co. Lo. co. N V (,) Year CO 0) 0 N CO ' LO 00) 00) 0 0 0 0 0 0 N—,—N N N N N N (1) O LS r OD 0) 0 ,— N CO ' LO (O r OD 0) (Z: 0 0 0 0 0 0 0 0 0 0 0 0 0 0 ai N N N N N N N N N N N N N N 0 0 N WETS 30th Percentile WETS 70th Percentile WETS A\erage C 0 2 a) N 0 O 0) c N N E a) c O a) _c tc C O E a) c O E c C a) E U a) Q O_ U a) te+ a) N c a) a) n Ct N a) I-F-4 Table I-F2. a) Q c a) a) a) a) a) E as Q a) E O V) a) a) O z ui a) a) U a) U Q E O N a) J cO O c as 92 U Q U a) L r-+ O (13 4- V1 Q a) O N •L a) a) co- 0 a) 2 l D O co o Q 2 ° Z 7(0 Q N co co co O co co V (O r- 00 (O .-C) N (NO V IN OM') V 1N- V l) CO N I� V N CO CO N N V CO 0) (O .- If) (O r- (O O) (O .-O O) V O N 00 M V 1m IN V V V IMn (MO l°f)) CO (NO V (NO (O 0 co .-O) C) 1� In mom C C C mom C C C Duck Creek Y O W 0 W ' ' ' ' '3 In 0) (O CO I� CO N CO CO I� CO N.- ,— O CO - O) In In 'I' (ON(O0)NNL)NOV Vn0VoOVnCn CO M 0 (ONO) N.- N 0O40 N (6 (6 (C C(6 C(6 Durham Creek N °) F 7 U 0 cO (0 In rn CO 0 O M M O V In CON O C) If) If) M N O If) c In In In c ,o- co moo O N 0O O If) O c co m (6 (6 (6 C C C (6 (6 (6 C C C Porter Creek Porter DCUT11 Creek O) V (O C) O) O) M O o0 V In In (O N n. V C) (O O) V (O m (O 1, O) O M O) O) (O In V N 1: N C) O 00 M V In In V In V In In C) ON O) O) m o0 In V C) ON O) O) In 00 In V (O (O N 1- M 0') (O In 1- (O (O N 1: (O 0') (O In 1- o) In 0') N O) meow V 1- In co,-0) - N .- (O C) C) M 1- to O) (O N 0') O) (O m o0 ,- V In In (O (O to .-O) - (O o0 d) M In V r M (O N 00 (O 0') m In 1- (O O (O O) N V CO M O V 1- (O N W "a 7 13 U 7 2 N W "a 7 E 0 7 2 co O V 00 . N..-r .-00 0') N O CO O If) C) V (O In N o0 M 1- M o0 N:00 O M V In O) N r V I- (') LC) N 00 (O 1- 00 1- N O to V O V V In 6M V N:(O (O 6(O V V In V V In In V In V (O CO V N .-1- N CO OCON:) C) (O V 00 V N .-.-00 N 0 C) (O V N 00 V V (O V (O If) Tooley Creek Tooley Long Creek* Creeka V 0o co In 0') M N. .- to N In m M 4 o V (OO N• W 3 Broomfield Swamp SCUTa Creek U rn rn O) - V )(0 rn cm.- mo rn rn rn O) - LC) V V O MOM rn rn mom N N (6 C C C rn rn mom N N (6 C C a PA2 Jacks Little Jacobs a Drinkwater Creek* Creeka Creek PA2 Creek V 1- co V O) r co co co °) N V IOn M V (OO V (O c(No((oCCor- 0') In V m V N V (O () If) V m V N V (O 0') m V m V N V (O () If) V m V N V (O V 1m .- V O (O V O (O .- V O (O V O (O V N m 1- 00 N m 1- o0 N m 1- 00 N m 1- 00 IN r-(o mcc000 (O N (O (O V 1. m m V m m (O m O In (O N r- r (O In 00 O (O N (O (O V N- m m V m m (O m O In (O N 1- r M to 00 O (O N (O (O V 1. m m V m m (O m O.-If) (O N r- r (O In 00 O (O N (O (O V N. m m V m m (O m O If) (O N 1- r (O to 00 O m IN V IMn 1m () (mmocoo - r N V (O In O N O mom N- N V (O In O N O mom .-r N V (O In O N O mom N- N V (O In 1- N 00 00 O O mom In c(NouM) M m O) V m V (6 (6 (6 C C C O N O) (O (O 00 .- to (O V m V (6 (6 (6 C C C 1- r (O 00 V O) M (O V woo - r 0') V (O In (6 N (6 C C C N V mom (O r to V (O In (6 N (6 C C C —Nco (O O 1- V () 1m Rain Gauge Location co W >- 00 O) O N O') V If) 0) 0) O O O O O O O O O O O O O O .-.-N N N N N N r- 00 O) O O O O O O O .-N M V If) (O r- 00 O) O N O O O O O O O O O O O CNN All Years Min Max Average Pre -Years (impact) Min Max Average Post- Years Min Max Average * Rainfall data from the closest alternative rain gauge is substituted in instances where the primary rain gauge is damaged or suspected of malfunction. I-F-5 G. Tar River Discharge The Tar River is approximately 215 miles long and travels generally in a southeast direction where it ends in the Pamlico Sound estuary. Below the US Highway 17 Bridge in Washington NC, the Tar River is called the Pamlico River. The Tar River discharge is measured at a gauge station located in Greenville, NC, approximately 35 miles north of PCS (Lat 35°37'00" Long 77°22'22"). Tar River discharge totals were highest in 1999 and 2003 and 2020 had the third highest total discharge since 1998 (Figure I-G1). Median Tar River discharge in 2020 was the second -highest since 1998 and mean Tar River discharge was the third -highest. I-G-1 0 m 0 m 1 co 0 74000 ---- 72000 =---- 70000 68000 — 66000 - 64000 = 62000 =- 600 00-- 58000 56000 =- 54000 -- 52000 50000 48000 - 46000 - 44000 = 42000 40000 -- 38000 36000 34000 -- 32000 30000 =- 28000 26000 24000 =7 22000 20000 — 18000 16000 14000 12000 10000 800a 6000 4000 2000 . 1 0 ,I Tar River Average Daily Discharge and PCS-Aurora Station 6N Daily Rainfall (1998-2005 and 2007-2020) ■ ,1 ■ III 1 l ' 1.0111'1 II Pr No monitoring t occured in 1 2006 cncncncnaomrnm00004rrrrnic'c.icir0)0) )vvvvu0)0)0)0)0)cfl0r-r-r-r0cncncna)6?6.) 0000rrrr04cisvc'10)0) cor ,J- - - - ko L.0to Lo LC) c00)0)0)r—r-1—r- 0-)0-)a,a,0000 a)6,g, 9:2g61CA61¢�1o00Q` 000Q� D0000000000Q` Do0Q� 000Q 0000Q� 0000000Q3` _ c.1CCl Nc` roCOI-r=ri7C7Nr01r—Coco``Cyrr6`1r=coCovCAr0)01r—rrlcl`v010006`1r=rrl0) CA0000)(0vciri.o0) r=in0)0)ac'1ocor=cov�+�+r 00cow_tici 0)0`or=u"iCOCAr'1omr-r=40000ACVoOCcovCAr ["lN NNN Nrr rr rrr r01[00001 CAN NN NNN CO-- NNN NCVN - N NNN NNr rr rr rr r` �v������C����"0)01Nc�c�rnN���C"�C�"��0)0)r u-".0C�--_ -0) -0�t`or�r a�vr`C�--_�C`���"�010)iCornc� CO Cr) N C'1 CO Cr) N CO CO 61 N CO CO 61 N COC7 r r N rfl m r N 111 CO r N In CO -a— N In m r r 0r4 r—O r4 r—Or �r—Or d-r-r r a]CVC)CO 0]N C` CO 6] N C`7 C001 N r0 C000 r r r r r r r r r r r r r r r r r r PCS-Aurora 6N Rainfall Tar River Average Daily Discharge 14.0 13.0 12.0 11.0 10.0 00 8.0 7.0 6.0 5.0 4.0 3.0 2.0 1.0 0-0 Rainfall (inches) Figure I-G1. Average daily Tar River discharge at Greenville, NC and daily rainfall at PCS Aurora Station 6 N during the years of the creek study. I-G-2