Upper-air Water Vapour

Water vapour is the predominant gaseous source of infrared opacity in the atmosphere, accounting for about 60% of the natural greenhouse effect for clear skies. Water vapour condenses to produce clouds, changing radiative properties and releasing latent heat that drives or modifies atmospheric circulation systems. Water vapour in the lower stratosphere, though present only in small amounts, is radiatively significant. Consequently, there is potential for additional climate change feedbacks through perturbations of the processes that control the amount of water vapour in the stratosphere, such as the Brewer-Dobson circulation that strongly influences tropical tropopause temperatures and the amount of CH4 oxidized in the stratosphere.

ECV Products and Requirements

These products and requirements reflect the Implementation Plan 2022 (GCOS-244).

The requirements are found in the complete 2022 ECVs Requirements document as well: ECV Upper-air Water Vapour.

ProductsWater Vapour Mixing Ratio in the
  Upper Troposphere and Lower StratosphereMiddle and Upper StratosphereMesosphere
 (*)UnitValuesValuesValues
Horizontal ResolutionGkm155050
B100500500
T50015001500
Vertical ResolutionGkm0.010.50.5
B0.111
T0.2533
Temporal ResolutionGh333
B666
T247272
TimelinessGh111
B120168168
T720720720
Required Measurement Uncertainty (2-sigma)Gppmv0.10.10.1
B0.250.250.25
T0.50.50.5
StabilityGppmv/decade<0.1<0.2<0.2
B0.10.20.2
T0.250.50.5
ProductsRelative Humiditiy in the 
  Boundary Layer  Free TroposphereUpper Troposphere and Lower Stratosphere
 (*)UnitValues UnitValuesValues
Horizontal ResolutionGkm15 km1515
B100 100100
T500 1000500
Vertical ResolutionGm1 km0.010.01
B10 0.10.1
T100 10.25
Temporal ResolutionGh<1 h<13
B6 66
T12 1224
TimelinessGh1 h11
B120 120120
T720 720720
Required Measurement Uncertainty (2-sigma)G%RH0.1 %RH0.10.5
B0.5 0.51
T1 12
StabilityG%RH/ decade0.1 %RH/ decade0.1<0.5
B0.5 0.50.5
T1 12
ProductsSpecific Humidity in the   Integrated Water Vapour
  Boundary Layer  Free Troposphere  
 (*)UnitValues UnitValues UnitValues
Horizontal ResolutionGkm15 km15 km25
B100 100 250
T500 1000 1000
Vertical ResolutionGm1 km0.01  -
B10 0.1 -
T100 1 -
Temporal ResolutionGh<1 h<1 h0.2
B1 1 1
T3 3 24
TimelinessGh1 h1 h24
B120 120 120
T720 720 720
Required Measurement Uncertainty (2-sigma)Gg Kg-10.1 g Kg-10.1 Kg m-30.1
B0.5 0.5 0.5
T1 1 1
StabilityGg Kg-1/ decade0.01 g Kg-1/ decade0.01 Kg m-3/ decade0.1
B0.05 0.05 0.2
T0.1 0.1 0.5

(*) Goal (G): an ideal requirement above which further improvements are not necessary. Breakthrough (B): an intermediate level between threshold and goal which, if achieved, would result in a significant improvement for the targeted application. The breakthrough value may also indicate the level at which specified uses within climate monitoring become possible. It may be appropriate to have different breakthrough values for different uses. Threshold (T): the minimum requirement to be met to ensure that data are useful

Data sources

This list provides sources for openly accessible data sets with worldwide coverage for which metadata is available. It is curated by the respective GCOS ECV Steward(s). The list does not claim to be complete. Anyone with a suitable dataset who wishes it to be added to this list should contact the abombelliatwmo [dot] int (GCOS Secretariat).

In Situ:


Reanalysis:


Satellite:

  • Satellite ECV Inventory by the CEOS/CGMS Working Group on Climate (WGClimate)
  • Aura Microwave Limb Sounder (MLS)
Upper air water vapour
النطاق:
Atmosphere
Subdomain:
Upper Atmosphere
Scientific Area:
Hydrosphere
ECV Steward:
Products:
Water Vapour Mixing Ratio in the Upper Troposphere and Lower Stratosphere, Water Vapour Mixing Ratio in the Middle and Upper Stratosphere, Water Vapour Mixing Ratio in the Mesosphere, Relative Humidity in the Boundary Layer, Relative Humidity in the Free Troposphere, Relative Humidity in the Upper Troposphere and Lower Stratosphere, Specific Humidity in the Boundary Layer, Specific Humidity in the Free Troposphere, Integrated Water Vapour