MbrlCatalogueTitleDetail

Do you wish to reserve the book?
Coastal Supra‐Permafrost Aquifers of the Arctic and Their Significant Groundwater, Carbon, and Nitrogen Fluxes
Coastal Supra‐Permafrost Aquifers of the Arctic and Their Significant Groundwater, Carbon, and Nitrogen Fluxes
Hey, we have placed the reservation for you!
Hey, we have placed the reservation for you!
By the way, why not check out events that you can attend while you pick your title.
You are currently in the queue to collect this book. You will be notified once it is your turn to collect the book.
Oops! Something went wrong.
Oops! Something went wrong.
Looks like we were not able to place the reservation. Kindly try again later.
Are you sure you want to remove the book from the shelf?
Coastal Supra‐Permafrost Aquifers of the Arctic and Their Significant Groundwater, Carbon, and Nitrogen Fluxes
Oops! Something went wrong.
Oops! Something went wrong.
While trying to remove the title from your shelf something went wrong :( Kindly try again later!
Title added to your shelf!
Title added to your shelf!
View what I already have on My Shelf.
Oops! Something went wrong.
Oops! Something went wrong.
While trying to add the title to your shelf something went wrong :( Kindly try again later!
Do you wish to request the book?
Coastal Supra‐Permafrost Aquifers of the Arctic and Their Significant Groundwater, Carbon, and Nitrogen Fluxes
Coastal Supra‐Permafrost Aquifers of the Arctic and Their Significant Groundwater, Carbon, and Nitrogen Fluxes

Please be aware that the book you have requested cannot be checked out. If you would like to checkout this book, you can reserve another copy
How would you like to get it?
We have requested the book for you! Sorry the robot delivery is not available at the moment
We have requested the book for you!
We have requested the book for you!
Your request is successful and it will be processed during the Library working hours. Please check the status of your request in My Requests.
Oops! Something went wrong.
Oops! Something went wrong.
Looks like we were not able to place your request. Kindly try again later.
Coastal Supra‐Permafrost Aquifers of the Arctic and Their Significant Groundwater, Carbon, and Nitrogen Fluxes
Coastal Supra‐Permafrost Aquifers of the Arctic and Their Significant Groundwater, Carbon, and Nitrogen Fluxes
Journal Article

Coastal Supra‐Permafrost Aquifers of the Arctic and Their Significant Groundwater, Carbon, and Nitrogen Fluxes

2024
Request Book From Autostore and Choose the Collection Method
Overview
Fresh submarine groundwater discharge (FSGD) can deliver significant fluxes of water and solutes from land to sea. In the Arctic, which accounts for ∼34% of coastlines globally, direct observations and knowledge of FSGD are scarce. Through integration of observations and process‐based models, we found that regardless of ice‐bonded permafrost depth at the shore, summer SGD flow dynamics along portions of the Beaufort Sea coast of Alaska are similar to those in lower latitudes. Calculated summer FSGD fluxes in the Arctic are generally higher relative to low latitudes. The FSGD organic carbon and nitrogen fluxes are likely larger than summer riverine input. The FSGD also has very high CO2 making it a potentially significant source of inorganic carbon. Thus, the biogeochemistry of Arctic coastal waters is potentially influenced by groundwater inputs during summer. These water and solute fluxes will likely increase as coastal permafrost across the Arctic thaws. Plain Language Summary Groundwater flows from land to sea, transporting freshwater, organic matter, nutrients, and other solutes that impact coastal ecosystems. However, along coasts of the rapidly‐warming Arctic, there is limited knowledge regarding how much fresh groundwater enters the ocean. Using field observations and numerical models, we show that groundwater flowing from tundra in northern coastal Alaska carries large amounts of freshwater, organic matter, and carbon dioxide to the Arctic lagoons during summer. These inputs are likely significant to coastal biogeochemical cycling and marine food webs. Groundwater discharge and the associated transport of dissolved materials are expected to increase due to longer periods of above‐zero temperatures that thaw frozen soils below the tundra. Key Points Summer fresh submarine groundwater discharge (FSGD) to the Alaskan Beaufort Sea is only 3%–7% of rivers but carries as much organic matter Summer FSGD delivers a median of 116 (interquartile range: 35–405) and 6 (2–21) kg/d per km dissolved organic carbon and nitrogen Fresh groundwater at the beach of Simpson Lagoon (SL) has a median PCO2 of ∼33,000 μatm implying substantial CO2 flux
Publisher
John Wiley & Sons, Inc,John Wiley and Sons Inc
Subject

Abrupt/Rapid Climate Change

/ Active Layer

/ Air/Sea Constituent Fluxes

/ Air/Sea Interactions

/ Aquifers

/ Asteroids

/ Atmospheric

/ Atmospheric Composition and Structure

/ Atmospheric Effects

/ Atmospheric Processes

/ Avalanches

/ Benefit‐cost Analysis

/ Biogeochemical cycles

/ Biogeochemical Cycles, Processes, and Modeling

/ Biogeochemical Kinetics and Reaction Modeling

/ Biogeochemistry

/ Biogeosciences

/ Carbon

/ Carbon cycle

/ Carbon dioxide

/ Climate and Interannual Variability

/ Climate Change and Variability

/ Climate Dynamics

/ Climate Impact

/ Climate Impacts

/ Climate Variability

/ Climatology

/ Coastal aquifers

/ coastal Arctic lagoons

/ Coastal ecosystems

/ Coastal plains

/ Coastal waters

/ Comets

/ Comets: Dust Tails and Trails

/ Computational Geophysics

/ Cryobiology

/ Cryohydrogeology

/ Cryosphere

/ Decadal Ocean Variability

/ Disaster Risk Analysis and Assessment

/ Earth System Modeling

/ Earthquake Ground Motions and Engineering Seismology

/ Effusive Volcanism

/ Explosive Volcanism

/ Fluxes

/ Food chains

/ Food webs

/ Freshwater

/ Freshwater ecosystems

/ Frozen food

/ Frozen ground

/ Frozen groundwater

/ General Circulation

/ Geodesy and Gravity

/ Geological

/ Global Change

/ Global Change from Geodesy

/ Gravity and Isostasy

/ Groundwater

/ Groundwater discharge

/ Groundwater flow

/ Groundwater/Surface Water Interaction

/ groundwater‐surface water interactions

/ Hydrological Cycles and Budgets

/ Hydrology

/ Impacts of Global Change

/ Informatics

/ Inland water environment

/ Inorganic carbon

/ Lagoons

/ Land/Atmosphere Interactions

/ Latitude

/ Marine Geology and Geophysics

/ Mass Balance

/ Mathematical models

/ Modeling

/ Mud Volcanism

/ Natural Hazards

/ Nitrogen

/ Numerical Modeling

/ Numerical models

/ Numerical Solutions

/ Nutrients

/ Ocean influence of Earth rotation

/ Ocean models

/ Ocean Monitoring with Geodetic Techniques

/ Ocean/Atmosphere Interactions

/ Ocean/Earth/atmosphere/hydrosphere/cryosphere interactions

/ Oceanic

/ Oceanography: Biological and Chemical

/ Oceanography: General

/ Oceanography: Physical

/ Oceans

/ Organic carbon

/ Organic matter

/ Other

/ Paleoceanography

/ Permafrost

/ Permafrost depth

/ Permafrost, Cryosphere, and High‐latitude Processes

/ Physical Modeling

/ Planetary Sciences: Comets and Small Bodies

/ Planetary Sciences: Solar System Objects

/ Policy Sciences

/ Radio Oceanography

/ Radio Science

/ Regional Climate Change

/ Regional Modeling

/ Research Letter

/ Risk

/ Sea Level Change

/ Sea Level: Variations and Mean

/ Seismology

/ Solid Earth

/ Solutes

/ submarine groundwater discharge

/ Summer

/ Surface Waves and Tides

/ Thaws

/ Theoretical Modeling

/ Tsunamis and Storm Surges

/ Tundra

/ Volcanic Effects

/ Volcanic Hazards and Risks

/ Volcano Monitoring

/ Volcano Seismology

/ Volcano/Climate Interactions

/ Volcanology

/ Water Cycles

/ Water discharge