Experimentos Espaciales de PMODWRC Para Medir La Constante Solar y La Influencia de Irradiance Solar...

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 Physikalisc h-Meteorologische s Observatorium Davos    1    2  .    3  .    2    0    0    7 PMOD 1907-2007 WRC since 1971 Two activities: Energy balance and influence of radiation on the t errestrial climate 3/4 Green house effect 3/ 4 Sun-Earth connection Research Space experiments of PMOD/WRC to measure the solar constant and the influence of the solar irradiance on the terrestrial climate Werner Schmutz PMOD/WRC ISPMSRS'07 12-14 March 2007 Davos, Switzerland  Overview 1

Transcript of Experimentos Espaciales de PMODWRC Para Medir La Constante Solar y La Influencia de Irradiance Solar...

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PMOD 1907-2007

WRC since 1971

Two activities:

Energy balance and influence

of radiation on the terrestrialclimate

3/4 Green house effect 

3/4 Sun-Earth connection 

Research

Space experiments of PMOD/WRCto measure the solar constant and

the influence of the solar irradiance

on the terrestrial climate

Werner Schmutz

PMOD/WRC

ISPMSRS'07 12-14 March 2007 Davos, Switzerland 

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Overview

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Absolutely calibrated

TSI observations

TIM/SORCE2003 -

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Past observations of the Total Solar Irradiance (TSI) and the TSI-composite

Why irradiance measurements

Why continue to measure TSI

Future irradiance observations

erview

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Traceable Radiometry Underpinning

Terrestrial- & Helio- Studies 

Mission proposal: TRUTHS  

Nigel Fox NPL

[email protected] 

James Aiken Plym Mar Lab

Xavier Briottet ONERA

John Barnett Ox univ.

Steve Groom Plym Mar Lab

Claus Frohlich PMOD/WRC

Jo Haigh Imp CollOlivier Hagolle CNES Hugh

Kieffer USGS

Judith Lean NRL

John Martin NPL

David Pollock U of Alab.

Mike Sandford RAL

Michael Schaepman U of Zur

Werner Schmutz PMOD/WRC

Keith Shine Uni of Read

Phil Teillet CCRS

Theo Theocharous NPL

Kurtis Thome U of Ariz

Terry Quinn BIPM

Michel Verstraete JRC(Italy)

Emma Woolliams NPL

Ed Zalewski U of Ariz

confidence.

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,

- ns rmens c ange 

and prepar i n -o r b i

Difficulties:- Bias bt 

MIS

A side note: Need for improved Quality Assurance!

Courtesy of Nigel Fox

. ex  

WMO areg

debate

2 dedicate d t o c a l i b r a t i o n e e n t  an racea y pro ems

No consistent st 

e

proposing

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TSI – including TIM/SORCE

 Absolute measurements cannot be used toconstruct a long-term record

Æ Merge to a relative composite 

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TSI – comparisons of differentcomposites

Courtesy of Claus Fröhlich

Different composites predictdifferent long-term trends:

erview

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's

re

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Why irradiance measurements?

  Space Climate: 

Long term rcord of the Solr Irradince Onlong term, it is not known what dominates, secular hang f Total Solr Irradiance or Influence of the long-term variations on the chem

mposit ion of he upp t thspectrl (UV) variationpropagation to the tropos 

But: although UV variations are much larger (up to climate

100%) all spectral variations are highly correlatedto TSI variations

n s or ermIUGG 2007: Rozano E Ega tosphe re i sd Mitg f t  

i m ulation of theSession MS020p temperaturerespose to the soar rradiance UV(Ly-α and 220 nm Herzberg band)rradiance Solar Activity and its Influences on the

?

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What is the influence of the Sun on the climate?

Graphics: Dr. J. Beer EAWAG, Switzerland

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Climate Anomaliesversus solar influence

River Thames in London 1813/1814

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Predicted long-term trend of 

TSI 100 years

Different “educated”

guesses!

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Three minima in the latest

(August 2006) version of the PMOD-composite

T p r n m 0 1 5W / m 2 ( = 0 p p m

irradiance measurements at theowe than the previus

Th th ii t i thi thighest possible accuracy!within ±0.08 W/m

2(0006% or 60

ÎSolution: twin instrument

experiment as VIRGO on SoHO

 and PREMOS+SOVAP on PICARDp p p

http:www.pmodwrc.ch follow the links:

4 projects 4 Solar Constant / Solar Irradiance    1   2 .   3 .   2

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Predicted long-term trend of TSI 400 years

Different “edu

guesses!

Suspected secular change of TSIneeds to be confirmedobservationallyted” 

4 requires long term observation

of several decades! 

erview

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Future TSI experiments

D I A R A D P M O 6 S P M L O I  SoHO launch 2. December 1995

VIRGO instruments

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Two absolute radiometers:- PMO6V (A & B)

- DIARAD (L & R)

Precision Filter Radiometer (blue, green, red)

Image of the Sun in the green light in low resolution

(12 pixels): 1 minute sampling ___________ 

VIRGO/SoHO:operational since 1996

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3/4 GLORY (USA: no launch date – ready tobe used as gap-filler) 

3/4 SOVIM/ISS and 

3/4 PREMOS+SOVAP/PICARD 

approved TSI experiments of PMOD/WRC

3/4 RAD/KuaFu-A only future TSI experiment

presently being considered 

erview

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Space experiments are beingbuilt in house at PMOD/WRC

today

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Space experiments of PMOD/WRC

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PICARD (PI G. Thuillier)PREMOS  – SOVAP  – SODISM

Total Solar Irradiance

Filter Radiometers

tellite

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Total Solar Irradiance

observations until 2012

CRIM III 2000 - ?

IRGO/SOHO 1996 - 2009 (+?

TIM/SORCE 2003 - 2008 - (?)

SOVIM/ISS 2008 – 2009 ?

PREMOS/PICARD 2009 – 2011

SOVAP/PICARD

(SDO 2008-2012 has no TSI instrument)

System may have TSI t –but are planned o startnot earlier than 2009 (?), more liky as 201

NPOESS 012

National P ig Operational Environmental

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 . .

 

Total Solar Irradianceobservations until 2012

 ACRIM III 2000 - ?

VIRGO/SOHO 1996 - 2007 - 2009

TIM/SORCE 2003 – 2008 - (GLORY?)

SOVIM/ISS 2007 - 2009 ?

PREMOS-TSI/PICARD 2009 - 2013 

SOVAP/PICARD

(SDO 2008-2012 has no TSI instrument)

KuaFu-A 2012 -irradiance measurement experiment comprising:Æ SIM = Solar Irradiance Monitor (CN: PI Daren Lu)  Æ DOR = Davos Observatory Radiometer (CH: Werner Schmutz) 

 . .

 

onc us ons

Short-term irradiance variations (days) are closely

related to variations of the chemical composition of theupper atmosphere

 Æ space weather: operational monitoring of TSI 

Long-term irradiance variations (tens to thousands of 

years) are probably (!) related to climate variations

Æ space climate: secular long term change of TSI 

TSI observations are most likely continuous andoverlapping until about 2012

RAD/KuaFu-A would be a matching continuation

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Integration of LYRA

on PROBA2

5.3.2007

Thank you for your attention!