Characteristics of Rain and Sea Spray Droplet Size Distribution at a Marine Tower

The effects of sea spray on open-ocean rainfall measurements-the drop size distribution (DSD) and rainfall intensities-were studied using a state-of-the-art optical disdrometer. The number of rain droplets less than 1 mm in diameter is affected by several factors, including the type of rainfall and...

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Main Authors: Hiroki Okachi, Tomohito J. Yamada, Yasuyuki Baba, Teruhiro Kubo
Format: Article
Language:English
Published: MDPI AG 2020-11-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/11/11/1210
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author Hiroki Okachi
Tomohito J. Yamada
Yasuyuki Baba
Teruhiro Kubo
author_facet Hiroki Okachi
Tomohito J. Yamada
Yasuyuki Baba
Teruhiro Kubo
author_sort Hiroki Okachi
collection DOAJ
description The effects of sea spray on open-ocean rainfall measurements-the drop size distribution (DSD) and rainfall intensities-were studied using a state-of-the-art optical disdrometer. The number of rain droplets less than 1 mm in diameter is affected by several factors, including the type of rainfall and seasonality. Over the ocean, small rain and large sea spray droplets co-exist in the same diameter size class (0.072 to 1000 mm); hence, sea spray creates uncertainty when seeking to characterize the drop size distribution (DSD) of rain droplets over the ocean. We measured droplet sizes at a marine tower using a state-of-the-art optical disdrometer, a tipping-bucket rain gauge, a wind anemometer, and a time-lapse camera, over a period that included typhoon Krosa of 2019. The number of rain droplets of diameter less than 1 mm increased monotonically as the horizontal wind speed became stronger. Thus, the shape parameter <i>μ</i> of the Ulbrich distribution decreased. This decreasing trend can be recognized as an increase in sea spray. During no-rainfall hours (indicated by rain gauges on the ocean tower and nearby land), sea spray DSDs were obtained at various horizontal wind speeds. Furthermore, the proportions of sea spray to rainfall at different rainfall intensities and horizontal wind speeds were determined; at a horizontal wind speed of 16 to 20 m s<sup>−1</sup>, the average sea spray proportions were 82.7%, 19.1%, and 5.3% during total rainfall periods of 2.1 mm h<sup>−1</sup>, 8.9 mm h<sup>−1</sup>, and 32.1 mm h<sup>−1</sup>, respectively. Representation of sea spray DSDs, as well as rainfall DSDs, is a key element of calculating real rainfall intensities over the open ocean.
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spelling doaj.art-7fee30e7880d4ccbaf3436463bee6f3c2023-11-20T20:20:45ZengMDPI AGAtmosphere2073-44332020-11-011111121010.3390/atmos11111210Characteristics of Rain and Sea Spray Droplet Size Distribution at a Marine TowerHiroki Okachi0Tomohito J. Yamada1Yasuyuki Baba2Teruhiro Kubo3Graduate School of Engineering, Hokkaido University, N13 W8, Kita-ku, Sapporo, Hokkaido 060-9628, JapanFaculty of Engineering, Hokkaido University, N13 W8, Kita-ku, Sapporo, Hokkaido 060-9628, JapanDisaster Prevention Research Institute, Kyoto University, 2500-106, Katata, Shirahama, Nishimuro, Wakayama 649-2201, JapanDisaster Prevention Research Institute, Kyoto University, 2500-106, Katata, Shirahama, Nishimuro, Wakayama 649-2201, JapanThe effects of sea spray on open-ocean rainfall measurements-the drop size distribution (DSD) and rainfall intensities-were studied using a state-of-the-art optical disdrometer. The number of rain droplets less than 1 mm in diameter is affected by several factors, including the type of rainfall and seasonality. Over the ocean, small rain and large sea spray droplets co-exist in the same diameter size class (0.072 to 1000 mm); hence, sea spray creates uncertainty when seeking to characterize the drop size distribution (DSD) of rain droplets over the ocean. We measured droplet sizes at a marine tower using a state-of-the-art optical disdrometer, a tipping-bucket rain gauge, a wind anemometer, and a time-lapse camera, over a period that included typhoon Krosa of 2019. The number of rain droplets of diameter less than 1 mm increased monotonically as the horizontal wind speed became stronger. Thus, the shape parameter <i>μ</i> of the Ulbrich distribution decreased. This decreasing trend can be recognized as an increase in sea spray. During no-rainfall hours (indicated by rain gauges on the ocean tower and nearby land), sea spray DSDs were obtained at various horizontal wind speeds. Furthermore, the proportions of sea spray to rainfall at different rainfall intensities and horizontal wind speeds were determined; at a horizontal wind speed of 16 to 20 m s<sup>−1</sup>, the average sea spray proportions were 82.7%, 19.1%, and 5.3% during total rainfall periods of 2.1 mm h<sup>−1</sup>, 8.9 mm h<sup>−1</sup>, and 32.1 mm h<sup>−1</sup>, respectively. Representation of sea spray DSDs, as well as rainfall DSDs, is a key element of calculating real rainfall intensities over the open ocean.https://www.mdpi.com/2073-4433/11/11/1210rain dropsea spraysize distributionmarine observationextreme weather event
spellingShingle Hiroki Okachi
Tomohito J. Yamada
Yasuyuki Baba
Teruhiro Kubo
Characteristics of Rain and Sea Spray Droplet Size Distribution at a Marine Tower
Atmosphere
rain drop
sea spray
size distribution
marine observation
extreme weather event
title Characteristics of Rain and Sea Spray Droplet Size Distribution at a Marine Tower
title_full Characteristics of Rain and Sea Spray Droplet Size Distribution at a Marine Tower
title_fullStr Characteristics of Rain and Sea Spray Droplet Size Distribution at a Marine Tower
title_full_unstemmed Characteristics of Rain and Sea Spray Droplet Size Distribution at a Marine Tower
title_short Characteristics of Rain and Sea Spray Droplet Size Distribution at a Marine Tower
title_sort characteristics of rain and sea spray droplet size distribution at a marine tower
topic rain drop
sea spray
size distribution
marine observation
extreme weather event
url https://www.mdpi.com/2073-4433/11/11/1210
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AT tomohitojyamada characteristicsofrainandseaspraydropletsizedistributionatamarinetower
AT yasuyukibaba characteristicsofrainandseaspraydropletsizedistributionatamarinetower
AT teruhirokubo characteristicsofrainandseaspraydropletsizedistributionatamarinetower