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Title: HadISDH: an updateable land surface specific humidity product for climate monitoring

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 permore » 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.« less

Authors:
 [1];  [2]; ORCiD logo [1];  [3];  [4];  [4];  [5];  [1]
  1. Met Office Hadley Centre, Exeter (United Kingdom)
  2. National Oceanic and Atmospheric Administration (NOAA), Asheville, NC (United States). National Climatic Data Center
  3. North Carolina Central Univ., Asheville, NC (United States). Cooperative Inst. for Climate and Satellites North Carolina; National Oceanic and Atmospheric Administration (NOAA), Asheville, NC (United States). National Climatic Data Center
  4. National Physical Lab., Teddington (United Kingdom)
  5. Univ. of East Anglia, Norwich (United Kingdom); King Abdulaziz Univ., Jeddah (Saudi Arabia)
Publication Date:
Research Org.:
Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). Oak Ridge Leadership Computing Facility (OLCF)
Sponsoring Org.:
USDOE Office of Science (SC)
OSTI Identifier:
1565097
Grant/Contract Number:  
SC0005689
Resource Type:
Accepted Manuscript
Journal Name:
Climate of the Past
Additional Journal Information:
Journal Volume: 9; Journal Issue: 2; Journal ID: ISSN 1814-9332
Publisher:
European Geophysical Union - Copernicus
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; Geology; Meteorology & Atmospheric Sciences

Citation Formats

Willett, K. M., Williams, 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. United States: N. p., 2013. Web. doi:10.5194/cp-9-657-2013.
Willett, K. M., Williams, C. N., Dunn, R. J. H., Thorne, P. W., Bell, S., de Podesta, M., Jones, P. D., & Parker, D. E. HadISDH: an updateable land surface specific humidity product for climate monitoring. United States. doi:10.5194/cp-9-657-2013.
Willett, K. M., Williams, C. N., Dunn, R. J. H., Thorne, P. W., Bell, S., de Podesta, M., Jones, P. D., and Parker, D. E. Thu . "HadISDH: an updateable land surface specific humidity product for climate monitoring". United States. doi:10.5194/cp-9-657-2013. https://www.osti.gov/servlets/purl/1565097.
@article{osti_1565097,
title = {HadISDH: an updateable land surface specific humidity product for climate monitoring},
author = {Willett, K. M. and Williams, C. N. and Dunn, R. J. H. and Thorne, P. W. and Bell, S. and de Podesta, M. and Jones, P. D. and Parker, D. E.},
abstractNote = {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.},
doi = {10.5194/cp-9-657-2013},
journal = {Climate of the Past},
number = 2,
volume = 9,
place = {United States},
year = {2013},
month = {3}
}

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