Hypoxia in the Baltic Sea: The Past, the Present and the Future, Daniel Conley

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Hypoxia in the Baltic Sea: The Past, the Present and the Future Daniel Conley with help from many others… Department of Geology Lund University, Sweden Email: [email protected] Twitter: @DanielJConley Supported by: BalticSea2020, BONUS (HYPER, COCOA), FORMAS Multistressors, Pew Marine Conservation Fellowship

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Hypoxia in the Baltic Sea and in the coastal zone Hypoxia in the past “Geoengineering” approaches

Transcript of Hypoxia in the Baltic Sea: The Past, the Present and the Future, Daniel Conley

Page 1: Hypoxia in the Baltic Sea: The Past, the Present and the Future, Daniel Conley

Hypoxia in the Baltic Sea:

The Past, the Present and the Future

Daniel Conley with help from many others…

Department of Geology

Lund University, Sweden

Email: [email protected]

Twitter: @DanielJConley

Supported by: BalticSea2020, BONUS (HYPER, COCOA),

FORMAS Multistressors, Pew Marine Conservation Fellowship

Page 2: Hypoxia in the Baltic Sea: The Past, the Present and the Future, Daniel Conley

Introduction

Hypoxia in the Baltic Sea and in the coastal zone

Hypoxia in the past

“Geoengineering” approaches

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Larger than the size of Denmark (43,000 km2)

Area with hypoxia averages ca. 49,000 km2

Hypoxia O2 < 2 mg/L

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Changes in hypoxia area with time

Carstensen et al. 2014 PNAS

No relationship to “major inflows” of saltwater

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Mininum oxygen

concentrations

(1955-2009)

Conley et al. 2011

ES&T

215 sites out of 613

coastal units have

experienced hypoxia

(O2 < 2 mg/l)

…and there is a trend

for decreasing O2

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Hypoxia in the recent past

from geological data

(laminated sediments)

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Hypoxia during the Holocene (the last c. 10 000 yrs)

Sediment stratigraphy

Zillén et al. 2008 Zillén and Conley 2010

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Published in: Carolina P. Funkey; Daniel J. Conley; Nina S. Reuss; Christoph Humborg; Tom Jilbert;

Caroline P. Slomp; Environ. Sci. Technol. 2014, 48, 2598-2602. DOI: 10.1021/es404395a Copyright © 2014 American Chemical Society

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The response of the Baltic Sea to

nutrient reductions will take time

Are there technical solutions available?

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But why?

Time scale of improvement is long (decades)

- Geoengineering provides rapid improvements

Costs of nutrient reductions to society are enormous

- Geoengineering is a cheaper alternative

Popular in the media and politically attractive

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Can we add oxygen to the Baltic? (Conley et al. 2009, ES&T)

The hypoxic area (oxygen < 2 mg/l) averages 49,000 km2

Would require 2-6 million tons oxygen to be added each year

20,000-60,000 railway cars of liquid oxygen each year to

keep bottom waters oxic

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BOX-WIN (http://BOX-WIN.se) Baltic Sea oxygenation and floating windpower demonstrator

Who decides?

Espoo (EIA) Convention

and the “one-stop-shop” principle

Danish Energy Agency

HELCOM has said NO – Sept 2014

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Scientific questions:

How much would phosphorus be reduced?

How would the Baltic react to more inflow events?

Would destabilization of the water column allow

winter mixing to break through the halocline?

What would happen to phytoplankton, zooplankton and larve?

Consumer questions:

Cost are enormous to set up the system; installation

and maintenance costs should also be included.

Effect on shipping lanes?

Management concerns:

Would this reduce efforts and money for nutrient reductions?

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Perspectives

Nutrients inputs have stimulated the growth of algae creating

the largest human induced low oxygen zone in the world

AND

“Geoengineering” promises rapid improvements

BUT

The potential ecological effects could be devastating to the

Baltic Sea ecosystem

THEREFORE

We must focus on the prescribed nutrient reductions

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Tusen tack!