[1] Carbon dioxide clouds, which are speculated by models on solar and extra-solar planets, have been recently observed near the equator of Mars. The most comprehensive identification of Martian CO 2 ice clouds has been obtained by the near-IR imaging spectrometer OMEGA. CRISM, a similar instrument with a higher spatial resolution, cannot detect these clouds with the same method due to its shorter wavelength range. Here we present a new method to detect CO 2 clouds using near-IR data based on the comparison of H 2 O and CO 2 ice spectral properties. The spatial and seasonal distributions of 54 CRISM observations containing CO 2 clouds are reported, in addition to 17 new OMEGA observations. CRISM CO 2 clouds are characterized by grain size in the 0.5-2 mm range and optical depths lower than 0.3. The distributions of CO 2 clouds inferred from OMEGA and CRISM are consistent with each other and match at first order the distribution of high altitude (>60 km) clouds derived from previous studies. At second order, discrepancies are observed. We report the identification of H 2 O clouds extending up to 80 km altitude, which could explain part of these discrepancies: both CO 2 and H 2 O clouds can exist at high, mesospheric altitudes. CRISM observations of afternoon CO 2 clouds display morphologies resembling terrestrial cirrus, which generalizes a previous result to the whole equatorial clouds season. Finally, we show that morning OMEGA observations have been previously misinterpreted as evidence for cumuliform, and hence potentially convective, CO 2 clouds.