Flood or Drought: How Do Aerosols Affect Precipitation? (Articolo in rivista)

Type

• Articolo in rivista (Classe)
• Prodotto della ricerca (Classe)

Label

• Flood or Drought: How Do Aerosols Affect Precipitation? (Articolo in rivista) (literal)

Anno

• 2008-01-01T00:00:00+01:00 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi

• 10.1126/science.1160606 (literal)

Alternative label

• Rosenfeld, D., U. Lohmann, G.B. Raga, C.D. O’Dowd, M. Kulmala, S. Fuzzi, A. Reissell, M.O. Andreae (2008)
  Flood or Drought: How Do Aerosols Affect Precipitation?
  in Science (N. Y., N.Y.)
  (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori

• Rosenfeld, D., U. Lohmann, G.B. Raga, C.D. O’Dowd, M. Kulmala, S. Fuzzi, A. Reissell, M.O. Andreae (literal)

Pagina inizio

• 1309 (literal)

Pagina fine

• 1313 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume

• 321 (literal)

Rivista

• Science (Rivista)

Note

• Scopu (literal)
• ISI Web of Science (WOS) (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni

• Hebrew Univ Jerusalem, Inst Earth Sci, IL-91904 Jerusalem, Israel ETH, Inst Atmospher & Climate Sci, CH-8092 Zurich, Switzerland Univ Nacl Autonoma Mexico, Mexico City 04510, DF, Mexico Natl Univ Ireland Univ Coll Galway, Sch Phys, Environm Change Inst, Galway, Ireland Natl Univ Ireland Univ Coll Galway, Ctr Climate & Air Pollut Studies, Environm Change Inst, Galway, Ireland Univ Helsinki, Dept Phys, FIN-00014 Helsinki, Finland CNR, Ist Sci Atmosfera & Clima, I-40129 Bologna, Italy Max Planck Inst Chem, Biogeochem Dept, D-55020 Mainz, Germany (literal)

Titolo

• Flood or Drought: How Do Aerosols Affect Precipitation? (literal)

Abstract

• Aerosols serve as cloud condensation nuclei (CCN) and thus have a substantial effect on cloud properties and the initiation of precipitation. Large concentrations of human-made aerosols have been reported to both decrease and increase rainfall as a result of their radiative and CCN activities. At one extreme, pristine tropical clouds with low CCN concentrations rain out too quickly to mature into long-lived clouds. On the other hand, heavily polluted clouds evaporate much of their water before precipitation can occur, if they can form at all given the reduced surface heating resulting from the aerosol haze layer. We propose a conceptual model that explains this apparent dichotomy. (literal)

Prodotto di

• Chimica dell'atmosfera (TA.P02.010.003) (Modulo)
• Institute of atmospheric sciences and climate (ISAC) (Istituto)

Autore CNR

• SANDRO FUZZI (Unità di personale interno)

Incoming links:

Prodotto

• Institute of atmospheric sciences and climate (ISAC) (Istituto)
• Chimica dell'atmosfera (TA.P02.010.003) (Modulo)

Autore CNR di

• SANDRO FUZZI (Unità di personale interno)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi

• Science (Rivista)