stations:

6
Fig.1. Location of the study site (23-28 S, 130-140 W). The background image is the annual water clarity (measured by Euphotic depth, in meters, Lee et al 2007 algorithm) of 2008 (from OBPG).

Upload: gisela

Post on 12-Jan-2016

25 views

Category:

Documents


0 download

DESCRIPTION

Fig.1. Location of the study site (23-28 S, 130-140 W). The background image is the annual water clarity (measured by Euphotic depth, in meters, Lee et al 2007 algorithm) of 2008 (from OBPG). Stations:. Rrs-derived a(420) [m -1 ]. 1:1. (a). a(420) [m -1 ]. Rrs-derived a ph (420) [m -1 ]. - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Stations:

Fig.1. Location of the study site (23-28 S, 130-140 W). The background image is the annual water clarity (measured by Euphotic depth, in meters, Lee et al 2007 algorithm) of 2008 (from OBPG).

Page 2: Stations:

STB4_S1AA_L3a.mat

STB5_S1AA_L3a.mat

STB8_S1AA_L3a.matGyre4_S1AA_L3a.matgyre5_SAC_L3a.mat

Stations:

Fig.2. Comparison between remote-sensing inversions and values determined independently by other means, all at 420 nm. (a) total absorption; (b) particulate absorption; (c) gelbstoff absorption. Values for X-axis from Table 1 in Morel et al (2007).

0.006 0.008 0.010 0.012

0.006

0.008

0.010

0.012

a(420) [m-1]

ap(420) [m-1]

Rrs

-de

rive

d a

(42

0)

[m

-1]

0.001 0.002 0.003 0.004 0.0050.001

0.002

0.003

0.004

0.005

Rrs

-de

rive

d a

ph(4

20

) [

m-1]

0.001 0.002 0.003 0.004

0.001

0.002

0.003

0.004

ag(420) [m-1]

Rrs

-de

rive

d a

dg(4

20

) [

m-1]

1:1

1:11:1

(a)

(c)(b)

Page 3: Stations:

1/1/98 1/1/99 1/1/00 1/1/01 1/1/02 1/1/03 1/1/04 1/1/05 1/1/06 1/1/07 1/1/080.0005

0.0006

0.0007

0.0008

0.0009

Fig.3. Monthly times series of primary optical properties derived from SeaWiFS observations (1/1998 – 12/2007). (a): phytoplankton absorption coefficient (443 nm); (b) detritus/gelbstoff absorption coefficient (443 nm); (c) “particle” backscattering coefficient (555 nm). Overlaid on (a) and (b) are empirical models (open sysmbol) to highlight the seasonal and interannual dynamics.

1/1/98 1/1/99 1/1/00 1/1/01 1/1/02 1/1/03 1/1/04 1/1/05 1/1/06 1/1/07 1/1/08

0.003

0.004

0.005

0.006Datapattern

1/1/98 1/1/99 1/1/00 1/1/01 1/1/02 1/1/03 1/1/04 1/1/05 1/1/06 1/1/07 1/1/080.000

0.001

0.002

0.003datapattern

a ph(

44

3)

[m

-1]

a dg(

44

3)

[m

-1]

Month-Year Month-Year

Month-Year

b bp(

55

5)

[m

-1]

(a) (b)

(c)

Page 4: Stations:

1/1/981/1/991/1/001/1/011/1/021/1/031/1/041/1/051/1/061/1/071/1/080.000

0.001

0.002

0.003

0.004

backgroundreg.intensityreg.

1/1/98 1/1/99 1/1/00 1/1/01 1/1/02 1/1/03 1/1/04 1/1/05 1/1/06 1/1/07 1/1/080.0000

0.0005

0.0010

0.0015

0.0020

0.0025

0.0030

backgroundreg.intensityreg.

R2 = 0.108

Fig.4. Internannual dynamics of the background and seasonal intensity of aph and adg.

a ph(

44

3)

[m

-1]

Month-Year

R2 = 0.122

a dg(

44

3)

[m

-1]

Month-Year

R2 = 0.423

R2 = 0.042

Page 5: Stations:

21 22 23 24 25 26 27 280.000

0.001

0.002

0.003

21 22 23 24 25 26 27 280.002

0.003

0.004

0.005

0.006

SST [oC]

a ph(

44

3)

[m

-1]

a dg(

44

3)

[m

-1]

SST [oC]

Fig.5. Relationship between SST and aph (left), and between SST and adg (right) .

R2 = 0.106 R2 = 0.629

Page 6: Stations:

1/1/98 1/1/99 1/1/00 1/1/01 1/1/02 1/1/03 1/1/04 1/1/05 1/1/06 1/1/07 1/1/080.010

0.015

0.020

0.025

0.030

0.035

intensitybackground

Fig.6. (a) Monthly time series of chlorophyll-a concentration derived from SeaWiFS. Blue symbol and line for Chla derived from the aph results, with the formula from Bricaud et al (2004): aph(443) = 0.0654 Chla0.728. (b) As Fig.3, background and intensity of Chla, with Chla from the empirical OC4 algorithm.

1/1/98 1/1/99 1/1/00 1/1/01 1/1/02 1/1/03 1/1/04 1/1/05 1/1/06 1/1/07 1/1/080.00

0.01

0.02

0.03

0.04

0.05

Chla from aph

Chla from OC4

Ch

la

[mg

/m3 ]

Month-Year

Ch

la

[mg

/m3 ]

Month-Year