Table 1 Comparison of deep water buoys observed tropical cyclones

From: The role of enhanced velocity shears in rapid ocean cooling during Super Typhoon Nepartak 2016

Tropical cyclones

Mooring characteristics

L min

W max

Year

Name

C

Location of buoy

Depth

Parameters

1975

Eloise35

2

Gulf of Mexico

2541

T at 2, 50, 200, and 500 m; (u, v) at 50 m.

16

35

1988

Nelson36

2

Southeast of Japan

4900

T at 8 depths in the upper 100 m.

50

43.5

1995

Felix3

1

Bermuda

4567

T at 7 depths (upper 150 m); (u, v) at 25, 45, 71, and 106 m.

90

38

2003

Fabian3

3

Bermuda

4567

T at 16 depths (upper 1500 m); (u, v) profiles (upper 200 m).

102

54

2005

Nate3

1

Bermuda

4567

Same as Fabian in 2003.

123

39

2009

Choi-Wan5

1

Kuroshio Extension

6000

T at 20 depths (upper 525 m).

40

30

2010

Fanapi9

3

Western North Pacific

5450

T at 14 depths (upper 147 m).

68

18

2010

Megi9

5

Western North Pacific

5500

T at 10 depths (upper 148 m).

123

23.5

2014

Kalmaegi10

1

South China Sea

3990

T at 15 depths (upper 400 m); (u, v) profiles (upper 245 m).

32

23

2016

Nepartak

5

Western North Pacific

5490

T at 12 depths (upper 500 m); (u, v) at 25 and 75 m.

19

46.5

2016

Nepartak

5

Western North Pacific

4870

T at 12 depths (upper 500 m); (u, v) at 25 and 75 m.

6

44

  1. Column C means category based on the Saffir–Simpson scale, Depth is the water depth (in m) at where the buoy was anchored, Lmin is the closest distance (in km) from the buoy to the typhoon/hurricane eye center, and Wmax is buoy observed maximum wind speed (in m s−1)