Why Does Large Relative Humidity with Respect to Ice Persist in Cirrus Ice Clouds?

A. Bogdan; M. J. Molina

doi:10.1021/jp9063609

Why Does Large Relative Humidity with Respect to Ice Persist in Cirrus Ice Clouds?

A. Bogdan
, M. J. Molina

Research output: Contribution to journal › Article › Scientific › peer-review

Original language	English
Journal	Journal of Physical Chemistry A
Volume	113
Pages (from-to)	14123-14130
Number of pages	8
ISSN	1089-5639
DOIs	https://doi.org/10.1021/jp9063609
Publication status	Published - 2009
MoE publication type	A1 Journal article-refereed

Fields of Science

POLAR STRATOSPHERIC CLOUDS
LOW-TEMPERATURE CIRRUS
TROPICAL TROPOPAUSE
SULFURIC-ACID
HOMOGENEOUS NUCLEATION
RADIATIVE PROPERTIES
SUBVISIBLE CIRRUS
PHASE-TRANSITIONS
GLASSY WATER
NITRIC-ACID
114 Physical sciences
116 Chemical sciences

Access to Document

10.1021/jp9063609

Cite this

@article{d6e2e04fb0bf4d48a9dd755fbe63bba2,

title = "Why Does Large Relative Humidity with Respect to Ice Persist in Cirrus Ice Clouds?",

keywords = "POLAR STRATOSPHERIC CLOUDS, LOW-TEMPERATURE CIRRUS, TROPICAL TROPOPAUSE, SULFURIC-ACID, HOMOGENEOUS NUCLEATION, RADIATIVE PROPERTIES, SUBVISIBLE CIRRUS, PHASE-TRANSITIONS, GLASSY WATER, NITRIC-ACID, 114 Physical sciences, 116 Chemical sciences",

author = "A. Bogdan and Molina, \{M. J.\}",

year = "2009",

doi = "10.1021/jp9063609",

language = "English",

volume = "113",

pages = "14123--14130",

journal = "Journal of Physical Chemistry A",