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Cape Hatteras
the Confluence of the
South & Mid Atlantic Bight Provinces
and the Appalachians & the Gulf Stream
On Events and Implications
Part I
Len Pietrafesa, Shaowu Bao,
Tingzhuang Yan, Paul Gayes,
Jim Epps
The “confluence”
Is clearly depicted
In this AVHRR SST
Where 6o C waters
Meet 12o to 20o
Waters
And Cold, Dry Air
Masses encounter
Warm, Moist
Gulf Stream
Conditioned
Air Masses
Cape Hatteras has many special properties
Like multiple cross shelf fronts
And topographic influences,
Which induces SB and Slope
Upwelling ~ 10-1 cm/sec
Thus creating a very complex Air-Sea interaction system
And conditions for “explosive cyclogenesis”
=> D(D(T))/DXDZ = maximum baroclinicity =>
an atmospheric “bomb”
The spawning or further intensification of ETCs
left: The New England Blizzard of 2004
a) Onset of an ETC
b) of ~ 100 cm/sec
and waves of height
(O) 5-10 meters;
effecting huge
Shear Stresses =>
bottom resuspension
and lateral erosion
c) Note MAB waters
breeching Diamond
Shoals down into
Raleigh Bay
d) The system relaxes
After 7- 8 days
• So, ETCs carry heat northward… and
• drop heavy precipitation …and
• are characterized by southward to southwestward , i.e. northeasterly winds…hence
the term “Nor’Easters”
• which move blue crab juveniles from Chesapeake Bay to the south and into the
primary nurseries and settlement areas of Pamlico Sound via Oregon Inlet …and also…
• Bottom sediments are picked up by storm induced waves and currents and along with
the Chesapeake Bay Plume also enter the Inlets
• The sediments follow a track similar
to the crabs. The dirt ends up going
through Oregon Inlet and being
deposited on the backsides of the Outer
Bank, barrier island chain.
• This process allows these ephemeral
strips of sand to migrate west toward
the mainland, thus ensuring their
future during this period of sea level
rise
• Estuarine dependent finfish also move
across the shelf at the surface and the
interior into the Pamlico Sound
estuary
Numbers of ETCs
13 in 1998 and 24 in 2001
During a low ETC year there is less coastal water in the system
than during a high ETC year
With NE’ ly winds
Hydraulic Heads get created
Along the axes of the Inlets
And water pours into the system
0
2
4
6
8
10
12
1986 1988 1990 1992 1994 1996 1998 2000 2002
Catchpereffort Cluster 1 Cluster 2
Cluster 3 Cluster 4
-2
-1
0
1
2
3
4
5
6
7
8
1988 1990 1992 1994 1996 1998 2000 2002
Year Class
Y-O-YAbundanceIndex
0
1,000,000
2,000,000
3,000,000
4,000,000
5,000,000
6,000,000
7,000,000
AbundanceatAge(#s)
Y-O-Y
Age 1
Age 2
Variability within age classes. . .
2000 4000 6000 8000 10000
March Discharge
-1.0-0.50.00.51.0
Cluster4Abund
400 600 800 1000
Feb-Mar N-NE Winds
-0.50.00.51.0
Cluster4Abund
20 40 60 80 100 120
Feb-Mar E-SE Winds
-0.50.00.51.0
Cluster4Abund Cluster 4 vs. Environmental Factors
Comments:
Steve Ross?

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Cape Hatteras the Confluence of the South & Mid Atlantic Bight Provinces and the Appalachians & the Gulf Stream

  • 1. Cape Hatteras the Confluence of the South & Mid Atlantic Bight Provinces and the Appalachians & the Gulf Stream On Events and Implications Part I Len Pietrafesa, Shaowu Bao, Tingzhuang Yan, Paul Gayes, Jim Epps
  • 2. The “confluence” Is clearly depicted In this AVHRR SST Where 6o C waters Meet 12o to 20o Waters And Cold, Dry Air Masses encounter Warm, Moist Gulf Stream Conditioned Air Masses
  • 3. Cape Hatteras has many special properties Like multiple cross shelf fronts And topographic influences, Which induces SB and Slope Upwelling ~ 10-1 cm/sec
  • 4. Thus creating a very complex Air-Sea interaction system
  • 5. And conditions for “explosive cyclogenesis” => D(D(T))/DXDZ = maximum baroclinicity => an atmospheric “bomb”
  • 6.
  • 7.
  • 8. The spawning or further intensification of ETCs left: The New England Blizzard of 2004
  • 9. a) Onset of an ETC b) of ~ 100 cm/sec and waves of height (O) 5-10 meters; effecting huge Shear Stresses => bottom resuspension and lateral erosion c) Note MAB waters breeching Diamond Shoals down into Raleigh Bay d) The system relaxes After 7- 8 days
  • 10. • So, ETCs carry heat northward… and • drop heavy precipitation …and • are characterized by southward to southwestward , i.e. northeasterly winds…hence the term “Nor’Easters” • which move blue crab juveniles from Chesapeake Bay to the south and into the primary nurseries and settlement areas of Pamlico Sound via Oregon Inlet …and also… • Bottom sediments are picked up by storm induced waves and currents and along with the Chesapeake Bay Plume also enter the Inlets • The sediments follow a track similar to the crabs. The dirt ends up going through Oregon Inlet and being deposited on the backsides of the Outer Bank, barrier island chain. • This process allows these ephemeral strips of sand to migrate west toward the mainland, thus ensuring their future during this period of sea level rise • Estuarine dependent finfish also move across the shelf at the surface and the interior into the Pamlico Sound estuary
  • 11. Numbers of ETCs 13 in 1998 and 24 in 2001
  • 12. During a low ETC year there is less coastal water in the system than during a high ETC year
  • 13. With NE’ ly winds Hydraulic Heads get created Along the axes of the Inlets And water pours into the system
  • 14.
  • 15.
  • 16.
  • 17. 0 2 4 6 8 10 12 1986 1988 1990 1992 1994 1996 1998 2000 2002 Catchpereffort Cluster 1 Cluster 2 Cluster 3 Cluster 4
  • 18. -2 -1 0 1 2 3 4 5 6 7 8 1988 1990 1992 1994 1996 1998 2000 2002 Year Class Y-O-YAbundanceIndex 0 1,000,000 2,000,000 3,000,000 4,000,000 5,000,000 6,000,000 7,000,000 AbundanceatAge(#s) Y-O-Y Age 1 Age 2 Variability within age classes. . .
  • 19. 2000 4000 6000 8000 10000 March Discharge -1.0-0.50.00.51.0 Cluster4Abund 400 600 800 1000 Feb-Mar N-NE Winds -0.50.00.51.0 Cluster4Abund 20 40 60 80 100 120 Feb-Mar E-SE Winds -0.50.00.51.0 Cluster4Abund Cluster 4 vs. Environmental Factors Comments: Steve Ross?