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首页> 外文期刊>Deep-Sea Research >Remotely Sensed Sea-surface Chlorophyll And Poc Flux At Deep Gulf Of Mexico Benthos Sampling Stations
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Remotely Sensed Sea-surface Chlorophyll And Poc Flux At Deep Gulf Of Mexico Benthos Sampling Stations

机译:墨西哥湾深海Benthos采样站的遥感海表叶绿素和Poc流量

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摘要

Biweekly composite averages of the standing stock of sea-surface chlorophyll (SSC) were derived from SeaWiFS satellite ocean-color data at 44 benthic sampling stations occupied along the continental slope and rise by the Deep Gulf of Mexico Benthos (DGoMB) program. At the 22 DGoMB sites north of 26°N and west of 91°W in the NW Gulf of Mexico, annual average SSC was 0.19 mgm~(-3), ranging at most locations from annual highs of about 0.3 mg m~(-3) in November-February to lows of about 0.1 mg m~(-3) in May-August. Comparison of three years of SeaWiFS data (January 1998-December 2000) showed little inter-annual variation at these NW Gulf stations. In contrast, at the 22 NE Gulf sites north of 26°N and east of 91°W, SSC averaged 2.8 times higher than in the NW Gulf, showing also strong inter-annual variation. Maxima in the NE region occurred in November-February and also during summers. The summer maxima were associated with Mississippi River water transported offshore to the east and southward by anticyclonic eddies in the NE Gulf. The apparent increases in SSC in June-August at NE Gulf stations reached average monthly concentrations > 50% greater than in November-February. Based on a primary productivity model and a vertical flux model, the calculated export of particulate organic carbon (POC flux reaching the seafloor) was estimated as ~18 mg C m~(-2) day~(-1) at the 22 NE Gulf stations, and ~9 mg C m~(-2) day~(-1) at the 22 NW Gulf stations. These estimates are comparable to fluxes measured by benthic lander by others in the DGoMB program, which may drive the differences in west versus east bathymetric zonation and community structure of macrobenthos that were sampled with large box corers by others in the DGoMB program.
机译:海面叶绿素(SSC)常规存量的双周综合平均值来自于沿大陆坡占据并由墨西哥深湾本索斯(DGoMB)计划上升的44个底栖采样站的SeaWiFS卫星海洋颜色数据。在墨西哥西北西北26°N以北和91°W以西的22个DGoMB站点上,年平均SSC为0.19 mgm〜(-3),大部分地区的年最高SSC约为0.3 mg m〜(- 3)在11月至2月降低至5月至8月的约0.1 mg m〜(-3)。比较了三年的SeaWiFS数据(1998年1月至2000年12月),发现这些西北海湾站点的年际变化很小。相比之下,在26°N以北和91°W以东的22个东北海湾站点,南南合作平均水平是西北海湾的2.8倍,也显示出强烈的年际变化。东北地区的千里马发生在11月至2月以及夏季。夏季的最大值与东北海湾北部的反气旋涡旋将密西西比河的水运到东部和南部。 6月至8月在东北海湾地区的南南站明显增加,月平均浓度比11月至2月增加了50%以上。根据初级生产力模型和垂直通量模型,在墨西哥湾东北部22 NE,计算出的颗粒有机碳出口量(到达海底的POC通量)估计为〜18 mg C m〜(-2)day〜(-1)。台站,在墨西哥湾的22个西北站,约9 mg C m〜(-2)天〜(-1)。这些估计值可与DGoMB计划中底栖着陆器由其他人测量的通量相媲美,这可能会导致DGoMB计划中其他大型箱体取样的大型底栖动物的东西向测深分区和群落结构的差异。

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