Sentences with phrase «mm day»

SAT in units of °C per 30 years, precipitation in units of mm day − 1 per 30 years, and SLP contour interval of 1 hPa per 30 years with negative values dashed

There is a large range of uncertainty in the SAT regression values over northern Europe and Russia (1 — 3 °C), and in the P regression values over western Europe (0.15 — 0.75 mm day − 1).

In general, models tend to produce too many days with weak precipitation (< 10 mm day — 1) and too little precipitation overall in intense events (> 10 mm day — 1).

Get ready for grain: these were the 16 mm days of the show and as such the image always looks cheap and gritty, contradicting the idyllic intent of «Dawson's Creek»'s team of visualists.

New bone can be formed by stretching an osteotomy 1 mm a day.

Highest variance is seen in the rainfall during the monsoon with highs of 400 mm to the dry season with lows of 30 and 40 mm a day.

Multi-model mean changes in (a) precipitation (mm day — 1), (b) soil moisture content (%), (c) runoff (mm day — 1) and (d) evaporation (mm day — 1).

The larger changes reach 20 % or more of the simulated 1980 to 1999 values, which range from 1 to 5 mm day — 1 in wetter regions to below 0.2 mm day — 1 in deserts.

They found that most of the models produce light precipitation (10 mm day — 1).

Units are mm day - 1, °C and m s - 1 respectively; all data shown are from the 1958 - 2001 period.

The intensity of rainfall is likely to increase by 1 - 2 mm a day,» the report added.

Future 30 - year trends (2016 — 2045) in winter (a, b) SAT (°C per 30 years; color shading) and (c, d) precipitation (mm day − 1 per 30 years; color shading) from simulations 13 and 25 of the CESM1 Large Ensemble, chosen for their contrasting SLP trends (contours; interval = 1 hPa per 30 years with negative values dashed)

Panels e — h as in a — d but for precipitation (mm day − 1) in place of SAT.

c, d as in a and b but for precipitation (mm day − 1) in place of SAT.

The forced component of P trends is generally small (< 0.15 mm day - 1 in absolute value), with decreases over northern Africa and southern Europe and increases elsewhere (Fig. 2f).

Multi-model mean changes in surface air temperature (°C, left), precipitation (mm day — 1, middle) and sea level pressure (hPa, right) for boreal winter (DJF, top) and summer (JJA, bottom).

They found globally averaged differences between the current and the natural landscape of 1.2 mm day − 1 for precipitation and 0.6 mm day − 1 for moisture flux.