Not exact matches
a) global
mean thermosteric
sea level anomaly (b) and zonal
mean ocean temperature at 792.5 mtrs, 66 S (the Southern Ocean).
Climatologies of
sea level anomalies (> 0.05 m) and daily -
mean storm surges (> 0.3 m) are presented for the 1960 — 2010 cool seasons (October — April) along the East Coast of the United States.
iheartheidicullen @ 162: Sorry if my tone was intemperate, but really the SH and NH
sea ice trends have been analysed at length online by Tamino and others, over the last year or two, with the clear conclusion that the SH
anomaly trend is small (the
anomaly at the maximum last year was about 1.5 % of the
mean annual maximum, if I remember correctly) and not statistically significant (at the 95 %
level, I think), whereas the NH trend is large (tens of percent), long - lived, and statistically very significant indeed.
The stability and homogeneity of the C3S
sea level products is also ensured by the use of an homogeneous
mean reference to compute the
sea level anomalies for all missions.
Therefore, the altimeter
mean sea level provided here is not corrected for the TOPEX - A
anomaly.
Between 1993 and 1998, the global
mean sea level has been known to be affected by an
anomaly in TOPEX - A measurements (Valladeau et al., 2012; Watson et al., 2015, Dieng et al. (2017), Beckley et al., 2017).
SOI data are presented as annual
mean sea level pressure
anomalies at Tahiti and Darwin.
These
anomalies obviously had an effect on the global
mean of
sea levels.
The observed changes (lower panel; Trenberth and Fasullo 2010) show the 12 - month running
means of global
mean surface temperature
anomalies relative to 1901 — 2000 from NOAA [red (thin) and decadal (thick)-RSB- in °C (scale lower left), CO2 concentrations (green) in ppmv from NOAA (scale right), and global
sea level adjusted for isostatic rebound from AVISO (blue, along with linear trend of 3.2 mm / year) relative to 1993, scale at left in mm).