“…In particular, during the summer, these trends show diurnal asymmetric warming rates, where nighttime minimum temperatures ( T min ) have warmed faster than daytime maximum values ( T max ), thus decreasing the daily temperature range. The observed asymmetric warming during the last three decades at California coastal sites has been variously attributed to changes in cloud cover [ Nemani et al ., ], sea surface temperatures (SSTs) [ Goodridge , ; Karl et al ., ], increased upwelling [ Bakun ; Snyder et al ., ; McGregor et al ., ], land use changes for urbanization (LCLU) [ Mintz , ; Zhang , ; Chase et al ., ; Pielke et al ., ], irrigation [ Christy et al ., ; Bonfils and Lobell , ], greenhouse gases [ Duffy et al ., ; Walters et al ., ; Cayan et al ., ; Cordero et al ., ], Pacific Decadal Oscillation (PDO) [ Douville , ; LaDochy et al ., , ; Clark , ], and/or urban heat islands (UHIs) [ LaDochy et al ., ; Dai et al ., ; Kalnay and Cai , ; Diem et al ., ]. Furthermore, warming rates in California differ across seasons with higher warming in late winter/early spring and lowest in summer for daily maximum temperatures ( T max ) [ Bonfils et al ., ; Lebassi et al ., ].…”