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Cited by 257

The DOI matches its Crossref record; 13 of the 13 references it cites were found in a registry or an index.

Temperature and pressure dependence of the rain‐snow phase transition over land and ocean

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Dai, Aiguo·2008·Geophysical Research Letters

Abstract

The phase of precipitation is important for weather forecasts, land hydrology and remote sensing. To quantify the temperature and pressure dependence of snow frequency (F, in %) when precipitation occurs, we have analyzed 3‐hourly weather reports of surface air temperature (Ts, °C) and pressure (Ps), and snow and rain occurrences from over 15,000 land stations and available ship observations from 1977–2007. It is found that the phase transition occurs over a fairly wide range of temperature from about −2°C to +4°C over (low‐elevation) land and −3°C to +6°C over ocean. The F‐Ts relationship can be represented by a hyperbolic tangent: F(Ts) = a [tanh (b (Ts – c)) – d], with the slope parameter b close to 0.7 over land and 0.4 over ocean. The pressure‐dependence is only secondary and reflected in the parameters. Results show that snow occurs often (F > 50%) for Ts ≤ 1.2°C over land and Ts ≤ 1.9°C over ocean, and are non‐negligible (F > 5%) for Ts ≤ 3.8°C over land and Ts ≤ 5.5°C over ocean. This “warm bias” results from the falling of snowflakes into warmer surface layers, which is especially true over ocean. The warm bias is higher when air pressure is below ∼750 hPa because snow falls faster in thin air.

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Metadata

Authors
Dai, A.
Venue
Geophysical Research Letters
Published
2008-06-17
Volume
35
Issue
12
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W1649947482
Cited by
257
References
13
FWCI
0.42
Type
journal article
Language
en
Open access
bronze

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Dai, A. (2008). Temperature and pressure dependence of the rain‐snow phase transition over land and ocean. Geophysical Research Letters. https://doi.org/10.1029/2008gl033295

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