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A new tool for Radiative transfer within sea ice

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(1)

A new tool for

Radiative transfer within sea ice

Christian Katlein

Lovro Valcic

Simon Lambert-Girard Philipp Anhaus

Marcel Nicolaus Mario Hoppmann

(2)

Monitoring light in the sea ice system

Ecosystem

(3)

Advances in IOP understanding: a missing link

apparent optical properties

(albedo/transmittance) Radiative

transfer model inherent optical

properties

(absorption/scattering) Structural

optical model physical properties

(ice thickness, type,…)

climate model parameterizations

novel observation technologies:

In-ice measurements

(4)

Light chain

First prototype 2018

3.5m long

64 sensors each 5cm

RGB light sensors

Development ~10k€

Cost (chain only) ~2k€

Iridium SBD data transmission

Katlein, C., et al. (2020) New insights into radiative transfer in sea ice derived from autonomous ice internal measurements, in press in The Cryosphere

(5)

The Sensor: TCS3472

4 channel sensor RGB + clear light

Cosine response

IR filter

430-640nm (~PAR)

(6)

AO18 Deployment (20 August 2018)

(7)

Data from 2018 prototype

air

ice

water

Problems with addressing chip

snow

(8)

Profiles: 20 Aug – 3 Sep

(9)

Comparison to RAMSES station

(10)

Extinction coefficients

(11)

Sideward geometry: DISORT modeling

sideward planar irradiance total

scalar irradiance =

𝐸𝐸4𝜋𝜋 𝐸𝐸𝑠𝑠

𝑬𝑬

𝟒𝟒𝟒𝟒

≈ 𝟒𝟒 ⋅ 𝑬𝑬

𝑺𝑺

(12)

MOSAiC deployments

MYI coring site L3 (FYI) 2nd Floe (Pond)

FYI SYI

FYI

Changing surface Changing surface

Ocean Ocean Ocean

Pond

(13)

Spectral signals

Bloom?

Flushing/

Snowmelt

Algae on sensor

Color change

Algae change color:

species/ physiology Polarstern gap!

(14)

Summary

An easy to deploy low-cost tool for in-ice light measurements

Results comparable to traditional setups

In-ice measurements allow better IOP understanding

Equivalency of sideward and scalar irradiance

Spectral resolution allows ecosystem assment

Thankyou for your interest!

Katlein, C., et al. (2020) New insights into radiative transfer in sea ice derived from autonomous ice internal measurements, The Cryosphere

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