Short-term variability of aragonite saturation state in the central Mid-Atlantic Bight

Xu, Yuan‐Yuan; Cai, Wei‐Jun; Gao, Yonghui; Wanninkhof, Rik; Salisbury, Joseph; Chen, Baoshan; Reimer, Janet J.; Gonski, Stephen; Hussain, Najid

doi:10.1002/2017jc012901

Advanced Search

Select up to three search categories and corresponding keywords using the fields to the right. Refer to the Help section for more detailed instructions.

Search our Collections & Repository

Advanced Search
Custom Query

All these words:

For very narrow results

This exact word or phrase:

When looking for a specific result

Any of these words:

Best used for discovery & interchangable words

None of these words:

Recommended to be used in conjunction with other fields

Language:

Dates

Publication Date Range:

to

Document Data

Title:

Document Type:

Library

Collection:

Series:

People

Author:

Clear All

Query Builder

Query box

Clear All

For additional assistance using the Custom Query please check out our Help Page

i

Short-term variability of aragonite saturation state in the central Mid-Atlantic Bight

2017
By Xu, Yuan‐Yuan ; Cai, Wei‐Jun ; Gao, Yonghui ; ...
Source: Journal of Geophysical Research-Oceans, 122(5), 4274-4290.

[PDF-3.79 MB]

Details You May Also Like

Details:

Journal Title:

Journal of Geophysical Research: Oceans
Personal Author:

Xu, Yuan‐Yuan ; Cai, Wei‐Jun ; Gao, Yonghui ; Wanninkhof, Rik ; Salisbury, Joseph ; ... More +

Xu, Yuan‐Yuan ; Cai, Wei‐Jun ; Gao, Yonghui ; Wanninkhof, Rik ; Salisbury, Joseph ; Chen, Baoshan ; Reimer, Janet J. ; Gonski, Stephen ; Hussain, Najid Less -
NOAA Program & Office:

OAR (Oceanic and Atmospheric Research)
Description:

The uptake of anthropogenic carbon dioxide (CO2) from the atmosphere has resulted in a decrease in seawater aragonite saturation state ((arag)), which affects the health of carbonate-bearing organisms and the marine ecosystem. A substantial short-term variability of surface water (arag), with an increase of up to 0.32, was observed in the central Mid-Atlantic Bight off the Delaware and the Chesapeake Bays over a short period of 10 days in summer 2015. High-frequency underway measurements for temperature, salinity, percentage saturation of dissolved oxygen, oxygen to argon ratio, pH, fCO(2), and measurements based on discrete samples for pH, dissolved inorganic carbon, and total alkalinity are used to investigate how physical and biogeochemical processes contribute to the changes of (arag). Quantitative analyses show that physical advection and mixing processes are the dominant forces for higher (arag) in slope waters while biological carbon removal and CO2 degassing contribute to increased (arag) in shelf waters.
Source:

Journal of Geophysical Research-Oceans, 122(5), 4274-4290.
DOI:

https://doi.org/10.1002/2017jc012901
Document Type:

Journal Article
Rights Information:

Other
Compliance:

Submitted
Main Document Checksum:

[+]

urn:sha256:dd2fd0a8350c48ae3d43d02df65139ca70dd951d1befcf89f4837232eddc6474
Download URL:

https://repository.library.noaa.gov/view/noaa/18030/noaa_18030_DS1.pdf
File Type:

No Additional Files

More +

Short-term variability of aragonite saturation state in the central Mid-Atlantic Bight

Details:

Supporting Files

You May Also Like