Mlkevejen og Jordens klima Henrik Svensmark Dansk Rumforskningsinstitut

  • Slides: 13
Download presentation
Mælkevejen og Jordens klima Henrik Svensmark, Dansk Rumforskningsinstitut Email hsv@dsri. dk Københavns Universitet, 2002

Mælkevejen og Jordens klima Henrik Svensmark, Dansk Rumforskningsinstitut Email hsv@dsri. dk Københavns Universitet, 2002

Satellite Failures due to Space Weather Effects • Anomalies due to spacecraft surface and

Satellite Failures due to Space Weather Effects • Anomalies due to spacecraft surface and internal charging (Marecs, ECS, Meteosat, TELE-X, …. . ) • Latch-up induced failures (ESR-1, PRARE, Equator-S, …. . ) • SEU’s in linear circuits…(Anik 1 &2) • Solar Array problems/degradation (Tempo, Pan. Am, ECS, …. ) More recent satellite failures: • Telestar 401 – • TV links etc. . Galaxy IV – silenced 80% of pagers in North America More than 12 satellites lost due to Space Weather Effects Last 4 years space losses may have exceeded $500 million Commercial interests often do not allow anomaly reporting.

Damage to transformers Damage to a transformer at a power plant Delaware, New Jersey

Damage to transformers Damage to a transformer at a power plant Delaware, New Jersey Price: 10 mill USD Repair can take up to 1 year. In this particular case they were lucky to find a used one from a shut down plant. Took only 6 weeks to restore Sweden: simultaneous power loss in six 130 k. V power distribution lines Chicago: Five transformers in the Chicago area failed due to elevated geomagnetic activity

New Particle formation: Observations and Theory • Observed nucleation rates are much larger than

New Particle formation: Observations and Theory • Observed nucleation rates are much larger than predicted by classical binary (H 2 SO 4+H 2 O) nucleation theory • The functional dependence of the observed nucleation rate of [H 2 SO 4] is much weaker (~ [H 2 SO 4]2 )than predicted by classical binary (H 2 SO 4+H 2 O) nucleation theory (~ [H 2 SO 4]10 ) • Measured growth rates of freshly formed nanoparticles are about a factor of 10 higher than can be explained by H 2 SO 4 and its associated H 2 O and NH 3

Micro-physics: Why in the lower part of the atmosphere? t: Time to grow from

Micro-physics: Why in the lower part of the atmosphere? t: Time to grow from rc to r* DG ri T (sek) 400 300 200 100 0 rc r r* t ~ 200 sek for [H 2 SO 4] = 2. 5 107 pr cc 0 5 10 Ion-pair/cc/sek

Experimental evidence of enhanced aerosol formation caused by ionisation Natural level of ionisation Artificial

Experimental evidence of enhanced aerosol formation caused by ionisation Natural level of ionisation Artificial air N 2: O 2 = 4: 1 SO 2 = 300 ppb C 2 H 4 = 100 ppb O 3 = 160 ppb Vohra et al. , Atmos. Environment, 18, 1653 (1984)

Cosmic ray variations ionisation and aerosol formation Based on Numerical studies by Yu, 2001

Cosmic ray variations ionisation and aerosol formation Based on Numerical studies by Yu, 2001

CLOUD experimenet ved CERN

CLOUD experimenet ved CERN

Solaktivitet og Klima Kulstof-14 fra træ-ringe

Solaktivitet og Klima Kulstof-14 fra træ-ringe

IR Cloud properties and Cosmic rays Cosmic Ray - Low Cloud Top Temperature Correlation

IR Cloud properties and Cosmic rays Cosmic Ray - Low Cloud Top Temperature Correlation only found in low clouds Marsh and Svensmark, PRL 2000

Little Ice age (~ 1300 -1800) Documented in Europe Greenland Sargasso Sea Peru East

Little Ice age (~ 1300 -1800) Documented in Europe Greenland Sargasso Sea Peru East Africa Japan Caribbean Sea West Africa Taiwan and China South Africa USA Argentina

Ice-ages and spiral arms Cosmic ray flux is larger in spiral arms One revolution

Ice-ages and spiral arms Cosmic ray flux is larger in spiral arms One revolution take about 240 Mill years Spiral arm crossings every 140 Mill years

Ice-ages and spiral arms Nir Shaviv, PRL 2002

Ice-ages and spiral arms Nir Shaviv, PRL 2002