RT info:eu-repo/semantics/article
T1 Comparing Integrated Water Vapor Sun Photometer Observations Over the Arctic With ERA5 and MERRA‐2 Reanalyses
A1 Antuña‐Marrero, J. C.
A1 Román, R.
A1 Cachorro, V. E.
A1 Mateos, D.
A1 Toledano, C.
A1 Calle, A.
A1 Antuña‐Sánchez, J. C.
A1 Gonzalez, R.
A1 Antón, M.
A1 Vaquero‐Martínez, J.
A1 de Frutos Baraja, Á. M.
K1 Arctic
K1 2501 Ciencias de la Atmósfera
AB Atmospheric water vapor, a greenhouse gas, is increasing in the Arctic. It is a scientific challengeto understand the causes for this increase and determine adaptation and mitigation actions to confront itsclimatic effects. During the last decades, spatial and temporal coverage of water vapor satellite observations increased notably, and reanalysis water vapor estimates have steadily improved. However, the scarce spatial and temporal coverage in the Arctic of integrated water vapor (IWV) surface‐based observations limits the representativeness of satellite observations and reanalysis estimate validations. Recently, we validated sun photometer IWV (IWVsp) observations with IWV from radiosondes in the Arctic. Here, we compare the hourly means of IWVsp from 13 Arctic AERONET stations and the IWV from ERA‐5 and MERRA‐2 reanalyses. The comparison is conducted at hourly timescale for individual stations for two Arctic regions and for the whole Arctic. The comparison showed a moist bias of IWV from reanalyses with respect to IWVsp. The individual station wise pattern shows slightly better accuracy and precision for ERA5 than for MERRA‐2 also evident at the selected subregional scale. The differences of IWV from ERA5 and MERRA‐2 and IWVsp show no dependence on IWVsp nor the solar zenith angle. This study corroborates that IWVsp may be used for validations of satellite IWV observations and IWV reanalyses products.
PB American Geophysical Union
SN 2169-897X
YR 2025
FD 2025
LK https://uvadoc.uva.es/handle/10324/82295
UL https://uvadoc.uva.es/handle/10324/82295
LA eng
NO Journal of Geophysical Research: Atmospheres, 2025, vol 130, e2024JD041120.
NO Producción Científica
DS UVaDOC
RD 29-ene-2026