Clim. Past, 9, 657-677, 2013
www.clim-past.net/9/657/2013/
doi:10.5194/cp-9-657-2013
© Author(s) 2013. This work is distributed
under the Creative Commons Attribution 3.0 License.
HadISDH: an updateable land surface specific humidity product for climate monitoring
K. M. Willett1, C. N. Williams Jr.2, R. J. H. Dunn1, P. W. Thorne3, S. Bell4, M. de Podesta4, P. D. Jones5,6, and D. E. Parker1
1Met Office Hadley Centre, FitzRoy Road, Exeter, UK
2NOAA's National Climatic Data Center, Asheville, NC, USA
3Cooperative Institute for Climate and Satellites North Carolina, NCSU and NOAA's National Climatic Data Center, Asheville, NC, USA
4National Physical Laboratory, Teddington, UK
5Climatic Research Unit, University of East Anglia, Norwich, UK
6Center of Excellence for Climate Change Research/Dept of Meteorology, Faculty of Meteorology, Environment and Arid Land Agriculture, King Abdulaziz University, P.O. Box 80234, Jeddah 21589, Saudi Arabia

Abstract. HadISDH is a near-global land surface specific humidity monitoring product providing monthly means from 1973 onwards over large-scale grids. Presented herein to 2012, annual updates are anticipated. HadISDH is an update to the land component of HadCRUH, utilising the global high-resolution land surface station product HadISD as a basis. HadISD, in turn, uses an updated version of NOAA's Integrated Surface Database. Intensive automated quality control has been undertaken at the individual observation level, as part of HadISD processing. The data have been subsequently run through the pairwise homogenisation algorithm developed for NCDC's US Historical Climatology Network monthly temperature product. For the first time, uncertainty estimates are provided at the grid-box spatial scale and monthly timescale.

HadISDH is in good agreement with existing land surface humidity products in periods of overlap, and with both land air and sea surface temperature estimates. Widespread moistening is shown over the 1973–2012 period. The largest moistening signals are over the tropics with drying over the subtropics, supporting other evidence of an intensified hydrological cycle over recent years. Moistening is detectable with high (95%) confidence over large-scale averages for the globe, Northern Hemisphere and tropics, with trends of 0.089 (0.080 to 0.098) g kg−1 per decade, 0.086 (0.075 to 0.097) g kg−1 per decade and 0.133 (0.119 to 0.148) g kg−1 per decade, respectively. These changes are outside the uncertainty range for the large-scale average which is dominated by the spatial coverage component; station and grid-box sampling uncertainty is essentially negligible on large scales. A very small moistening (0.013 (−0.005 to 0.031) g kg−1 per decade) is found in the Southern Hemisphere, but it is not significantly different from zero and uncertainty is large. When globally averaged, 1998 is the moistest year since monitoring began in 1973, closely followed by 2010, two strong El Niño years. The period in between is relatively flat, concurring with previous findings of decreasing relative humidity over land.


Citation: Willett, K. M., Williams Jr., C. N., Dunn, R. J. H., Thorne, P. W., Bell, S., de Podesta, M., Jones, P. D., and Parker, D. E.: HadISDH: an updateable land surface specific humidity product for climate monitoring, Clim. Past, 9, 657-677, doi:10.5194/cp-9-657-2013, 2013.
 
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