Seasonal variability of bio-optical and physical properties in the Arabian Sea: October 1994-October 1995

T. Dickey, J. Marra, D. E. Sigurdson, R. A. Weller, C. S. Kinkade, S. E. Zedler, J. D. Wiggert, Chris Langdon

Research output: Contribution to journalArticle

96 Citations (Scopus)

Abstract

A mooring instrumented with optical and physical sensors within the upper 300 m was deployed for two consecutive 6-month periods (October 15, 1994 through October 20, 1995; sampling intervals of a few minutes) in the central Arabian Sea (15°30'N, 61°30'E). Both the Northeast Monsoon (November 1, 1994-February 15, 1995) and Southwest Monsoon (June 1-September 15, 1995) were observed. During the NE Monsoon, wind speeds averaged 6 m s-1 and reached up to 15 m s-1 during the SW Monsoon. Intermonsoon periods (Spring February 16-May 31, 1995; and Fall September 16-October 15, 1995) were characterized by weak and variable winds. Shortwave radiation and photosynthetically available radiation (PAR) displayed half-yearly cycles, peaking during the Intermonsoon periods. Two mixed-layer depth definitions have been used to describe our results. The first is based on a temperature difference of 0.1°C of the surface temperature, MLD(01°C), and the second is based on a difference of 1.0°C, MLD(1.0°C). The maximum Winter mixed layer depth (MLD(1.0°C) ~ 110 m) was deeper than the Summer mixed layer (MLD(1.0°C) 80 m), primarily because of surface cooling and convection. A half-yearly cycle in chlorophyll a was evident with greater values occurring during each Monsoon and into the Intermonsoon periods. High chlorophyll a values associated with cool mesoscale features were also apparent during each Monsoon. These mesoscale features and others have been identified using remotely sensed sea-surface height anomaly maps. Time-series of the 1% light level depth, h(1%) tracked the depth-integrated chlorophyll a. In general, h(1%) was deeper than MLD(1.0°C) during the latter half of the Spring Intermonsoon (SIM) (with low chlorophyll a periods) and shallower than MLD(1.0°C) during the latter portions of the Monsoons (high chlorophyll a periods). During the SIM, the penetrative components of net solar radiation at the base of the mixed layers, E(n)(MLD(1.0°C)) and E(n)(MLD(0.1°C)), reached values of ~40 and 75 W m-2, respectively, when the net surface heat flux was 120 W m-2. The highest mixed layer radiant heating rates occurred during the Intermonsoon periods with peak values greater than 0.2 and 0.1°C d-1 for MLD(0.1°C) and MLD(1.0°C), respectively. Our results indicate that biological variability is significant for the upper ocean heat budget of the central Arabian Sea during the SIM. The present results, in conjunction with those presented in Marra et al. (1998) and Honjo et al. (1998), demonstrate strong coupling of upper ocean biological processes with deep ocean particulate organic carbon fluxes. These collective results suggest that the timing and amplitudes of phytoplankton blooms associated with both seasonal stratification and eddies are quite well-correlated with relatively rapid export flux of organic carbon to the deep ocean.

Original languageEnglish
Pages (from-to)2001-2025
Number of pages25
JournalDeep-Sea Research Part II: Topical Studies in Oceanography
Volume45
Issue number10-11
DOIs
StatePublished - Aug 1 1998
Externally publishedYes

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Arabian Sea
optical properties
optical property
physical properties
monsoon
physical property
seasonal variation
chlorophyll
mixed layer
oceans
chlorophyll a
heat
upper ocean
algal blooms
wind speed
surface temperature
shortwave radiation
time series analysis
heat budget
sea surface height

ASJC Scopus subject areas

  • Aquatic Science
  • Geology
  • Oceanography

Cite this

Seasonal variability of bio-optical and physical properties in the Arabian Sea : October 1994-October 1995. / Dickey, T.; Marra, J.; Sigurdson, D. E.; Weller, R. A.; Kinkade, C. S.; Zedler, S. E.; Wiggert, J. D.; Langdon, Chris.

In: Deep-Sea Research Part II: Topical Studies in Oceanography, Vol. 45, No. 10-11, 01.08.1998, p. 2001-2025.

Research output: Contribution to journalArticle

Dickey, T. ; Marra, J. ; Sigurdson, D. E. ; Weller, R. A. ; Kinkade, C. S. ; Zedler, S. E. ; Wiggert, J. D. ; Langdon, Chris. / Seasonal variability of bio-optical and physical properties in the Arabian Sea : October 1994-October 1995. In: Deep-Sea Research Part II: Topical Studies in Oceanography. 1998 ; Vol. 45, No. 10-11. pp. 2001-2025.
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abstract = "A mooring instrumented with optical and physical sensors within the upper 300 m was deployed for two consecutive 6-month periods (October 15, 1994 through October 20, 1995; sampling intervals of a few minutes) in the central Arabian Sea (15°30'N, 61°30'E). Both the Northeast Monsoon (November 1, 1994-February 15, 1995) and Southwest Monsoon (June 1-September 15, 1995) were observed. During the NE Monsoon, wind speeds averaged 6 m s-1 and reached up to 15 m s-1 during the SW Monsoon. Intermonsoon periods (Spring February 16-May 31, 1995; and Fall September 16-October 15, 1995) were characterized by weak and variable winds. Shortwave radiation and photosynthetically available radiation (PAR) displayed half-yearly cycles, peaking during the Intermonsoon periods. Two mixed-layer depth definitions have been used to describe our results. The first is based on a temperature difference of 0.1°C of the surface temperature, MLD(01°C), and the second is based on a difference of 1.0°C, MLD(1.0°C). The maximum Winter mixed layer depth (MLD(1.0°C) ~ 110 m) was deeper than the Summer mixed layer (MLD(1.0°C) 80 m), primarily because of surface cooling and convection. A half-yearly cycle in chlorophyll a was evident with greater values occurring during each Monsoon and into the Intermonsoon periods. High chlorophyll a values associated with cool mesoscale features were also apparent during each Monsoon. These mesoscale features and others have been identified using remotely sensed sea-surface height anomaly maps. Time-series of the 1{\%} light level depth, h(1{\%}) tracked the depth-integrated chlorophyll a. In general, h(1{\%}) was deeper than MLD(1.0°C) during the latter half of the Spring Intermonsoon (SIM) (with low chlorophyll a periods) and shallower than MLD(1.0°C) during the latter portions of the Monsoons (high chlorophyll a periods). During the SIM, the penetrative components of net solar radiation at the base of the mixed layers, E(n)(MLD(1.0°C)) and E(n)(MLD(0.1°C)), reached values of ~40 and 75 W m-2, respectively, when the net surface heat flux was 120 W m-2. The highest mixed layer radiant heating rates occurred during the Intermonsoon periods with peak values greater than 0.2 and 0.1°C d-1 for MLD(0.1°C) and MLD(1.0°C), respectively. Our results indicate that biological variability is significant for the upper ocean heat budget of the central Arabian Sea during the SIM. The present results, in conjunction with those presented in Marra et al. (1998) and Honjo et al. (1998), demonstrate strong coupling of upper ocean biological processes with deep ocean particulate organic carbon fluxes. These collective results suggest that the timing and amplitudes of phytoplankton blooms associated with both seasonal stratification and eddies are quite well-correlated with relatively rapid export flux of organic carbon to the deep ocean.",
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T1 - Seasonal variability of bio-optical and physical properties in the Arabian Sea

T2 - October 1994-October 1995

AU - Dickey, T.

AU - Marra, J.

AU - Sigurdson, D. E.

AU - Weller, R. A.

AU - Kinkade, C. S.

AU - Zedler, S. E.

AU - Wiggert, J. D.

AU - Langdon, Chris

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N2 - A mooring instrumented with optical and physical sensors within the upper 300 m was deployed for two consecutive 6-month periods (October 15, 1994 through October 20, 1995; sampling intervals of a few minutes) in the central Arabian Sea (15°30'N, 61°30'E). Both the Northeast Monsoon (November 1, 1994-February 15, 1995) and Southwest Monsoon (June 1-September 15, 1995) were observed. During the NE Monsoon, wind speeds averaged 6 m s-1 and reached up to 15 m s-1 during the SW Monsoon. Intermonsoon periods (Spring February 16-May 31, 1995; and Fall September 16-October 15, 1995) were characterized by weak and variable winds. Shortwave radiation and photosynthetically available radiation (PAR) displayed half-yearly cycles, peaking during the Intermonsoon periods. Two mixed-layer depth definitions have been used to describe our results. The first is based on a temperature difference of 0.1°C of the surface temperature, MLD(01°C), and the second is based on a difference of 1.0°C, MLD(1.0°C). The maximum Winter mixed layer depth (MLD(1.0°C) ~ 110 m) was deeper than the Summer mixed layer (MLD(1.0°C) 80 m), primarily because of surface cooling and convection. A half-yearly cycle in chlorophyll a was evident with greater values occurring during each Monsoon and into the Intermonsoon periods. High chlorophyll a values associated with cool mesoscale features were also apparent during each Monsoon. These mesoscale features and others have been identified using remotely sensed sea-surface height anomaly maps. Time-series of the 1% light level depth, h(1%) tracked the depth-integrated chlorophyll a. In general, h(1%) was deeper than MLD(1.0°C) during the latter half of the Spring Intermonsoon (SIM) (with low chlorophyll a periods) and shallower than MLD(1.0°C) during the latter portions of the Monsoons (high chlorophyll a periods). During the SIM, the penetrative components of net solar radiation at the base of the mixed layers, E(n)(MLD(1.0°C)) and E(n)(MLD(0.1°C)), reached values of ~40 and 75 W m-2, respectively, when the net surface heat flux was 120 W m-2. The highest mixed layer radiant heating rates occurred during the Intermonsoon periods with peak values greater than 0.2 and 0.1°C d-1 for MLD(0.1°C) and MLD(1.0°C), respectively. Our results indicate that biological variability is significant for the upper ocean heat budget of the central Arabian Sea during the SIM. The present results, in conjunction with those presented in Marra et al. (1998) and Honjo et al. (1998), demonstrate strong coupling of upper ocean biological processes with deep ocean particulate organic carbon fluxes. These collective results suggest that the timing and amplitudes of phytoplankton blooms associated with both seasonal stratification and eddies are quite well-correlated with relatively rapid export flux of organic carbon to the deep ocean.

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