On 19-02-15 18:56, Jim Biard wrote:
Maarten,
It would, instead be something like this:
dimensions:
lon = 360;
lat = 180;
layer = 18;
vertices = 2;
variables:
float lat(lat);
lat:long_name = latitude;
lat:units = degrees_north;
lat:bounds = lat_bnds;
float
Maarten,
This is life with CF. Just to be sure I understand the details of the
problem, the vertical set of pressure values at one lat and lon is
different from the vertical set at a different lat and lon, correct? Is
there no metric (as in, not just an index) vertical coordinate that you
Hi,
A colleague has a question that left me without an answer. He writes:
I have a 3D ozone field with n_lon elements in longitude direction,
n_lat elements in latitude direction and n_layer elements in the
vertical direction. The corresponding pressure grid has the same number
of elements in
Maarten,
I believe that what your colleague should do is add a bounds variable
for the pressure and reduce the number of elements in the hPa coordinate
variable by one. The bounds variable provides a lower and upper bound
for each layer, so it captures the value currently being stored in the
Maarten,
It would, instead be something like this:
dimensions:
lon = 360;
lat = 180;
layer = 18;
vertices = 2;
variables:
float lat(lat);
lat:long_name = latitude;
lat:units = degrees_north;
lat:bounds = lat_bnds;
float lon(lon);
lon:long_name = longitude;
On 19-02-15 18:56, Jim Biard wrote:
Maarten,
It would, instead be something like this:
dimensions:
lon = 360;
lat = 180;
layer = 18;
vertices = 2;
variables:
float lat(lat);
lat:long_name = latitude;
lat:units = degrees_north;
lat:bounds = lat_bnds;
float
